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Dr. Arzu Javadova
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Existing Iran Oil and gas infrastructure.
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Recommandé
The new Government is targeting reforms and developments to radically transform the Iranian economy. Reforms are focused on: Better relationships with regional partners and the West Attracting foreign investment into the country Sustainable development of the petroleum sector: o Key for economic growth and welfare o Gradual removal of subsidies on energy Addressing and reduce unemployment Tightening fiscal policy to help the Central Bank with inflation Restructuring institutional decision making Stabilizing the Rial
Provinces of iran
Provinces of iran
Dr. Arzu Javadova
Using different public and private sources given field size distribution of Kurdsitan Iraq
Field size distribution of Kurdistan pptx
Field size distribution of Kurdistan pptx
Dr. Arzu Javadova
Reservoir modeling work flow chart
Reservoir modeling work flow chart
Reservoir modeling work flow chart
Dr. Arzu Javadova
The South Caspian Basin has many confirmed structures. It includes the offshore continuation of several major anticline trends extending from onshore side. The Umid Babek structure is one of the deepest structures of the Baku archipelago. It is strongly dislocated tectonically and is complicated by mud diapirism. Interpretation of 2D seismic data made it possible to determine the calculations for the area and depth in the Umid and Babek structures. The structures of Shah Deniz and Umid Babek are similar in terms of the history of their structural growth. Umid-Babek occupies the most advantageous position on the path of fluid migration from deep zones of depression and has favourable conditions for the accumulation and preservation of hydrocarbon deposits. U
РЕГИОНАЛЬНАЯ ГЕОЛОГИЯ_2021_3_испр финал1-10.pdf
РЕГИОНАЛЬНАЯ ГЕОЛОГИЯ_2021_3_испр финал1-10.pdf
Dr. Arzu Javadova
The results of reconnaissance studies within the Shakal and Halabja exploration blocks in Kurdistan are presented. Experimental studies were carried out using a mobile direct-prospecting technology, including modified methods of frequency-resonance processing and decoding of satellite images and photo images, vertical electric resonance scanning of the cross-section and a method of integral assessment of the oil and gas potential of large prospecting blocks and license areas. At the local survey site within the Shakal block, responses from oil, condensate, phosphorus and limestone were recorded. The lower boundary of the limestones was established at a depth of 4676 m. By scanning the cross-section from 2770 m, step 1 cm, the responses of oil from limestones were obtained from the intervals: 1) 2771-2794 m, 2) 2795.3-2815.45 m, 3) 2834.40-2854 m. During processing the image of the entire Halabja block, signals were recorded at the frequencies of oil, condensate, phosphorus gas, bacteria, sodium chloride and dolomite. At the 57 km hydrocarbon synthesis boundary, responses from oil, condensate and gas were recorded. When scanning the cross-section from 480 m to 4 km, step 50 cm, responses from oil were obtained from two intervals: 1) 1140-1200 m, and 2) 3310-3340 m. Within the local fragment of the block by scanning up to 5 km with a step of 1 m responses of oil from salt were recorded from the intervals: 1) 295-350 m, 2) 1190-1260 m, 3) 2015-2320 m). The response intervals within the 1st and 3rd horizons have been refined by scanning with a step of 5 cm. The results of experimental studies show that practical application of direct-prospecting methods and technologies will accelerate and optimize the exploration process for oil and gas.
RESULTS OF THE APPLICATION OF DIRECT-PROSPECTING TECHNOLOGY OF SATELLITE IMAG...
RESULTS OF THE APPLICATION OF DIRECT-PROSPECTING TECHNOLOGY OF SATELLITE IMAG...
Dr. Arzu Javadova
The results of the application of mobile direct-prospecting technology of frequency-resonance processing and interpretation of satellite images and photographs at the sites of hydrogen production, drilling wells, as well as within areas of hydrogen degassing in various regions are presented. Experimental reconnaissance studies were carried out to study the features of the deep structure of the hydrogen degassing areas. The developed mobile and low-cost technology include modified methods of satellite images and photo-images frequency-resonance processing and decoding, vertical electric-resonance scanning of a cross-section, as well as a method of integrated assessment of oil and gas potential of large prospecting blocks and license areas. Separate methods of direct-prospecting technology are based on the principles of the “substance” paradigm of geophysical research, the essence of which is searching for a specific substance - oil, gas, gas condensate, etc. The materials of instrumental measurements indicate that in regions of basalt volcano's location with roots at different depths, signals at hydrogen frequencies are almost always recorded. When scanning the cross-section, responses from hydrogen are recorded from the upper edges of basaltic volcanoes to their roots. It can be assumed that basaltic volcanoes are a kind of channel through which hydrogen migrates to the upper horizons of the cross-section and further into the atmosphere. Within many basaltic volcanoes at a depth of 68 km, deep (living) water is synthesized. Hydrogen-rich water is curative and can be used for wellness purposes. All surveyed zones of longevity on Earth are located within basalt volcanoes, in which water synthesized at a depth of 68 km migrates to the surface and is used for water supply. Hydrogen deposits can be formed by basaltic volcanoes in adjacent sealed reservoirs. Within some survey areas, responses at hydrogen frequencies from limestones, dolomites, and marls were recorded at shallow depths. Hydrogen deposits formed near basalt volcanoes in different types of reservoirs can be discovered and localized during areal exploration using proven methods. Direct-prospecting technology can also be used to study reservoirs in crystalline rocks (basalts including). Detailed studies and wells drilling in promising areas can be planned and carried out for hydrogen and living water at the same time. The result of the investigation indicates the advisability of using direct-prospecting methods of frequency-resonance processing of satellite images to detect zones of hydrogen accumulation in areas of basalt volcanoes location, as well as in areas of hydrogen degassing. The use of mobile and low-cost technology will significantly speed up the exploration process for hydrogen, as well as reduce the financial costs for its implementation.
Presentation1 final shortened.pdf
Presentation1 final shortened.pdf
Dr. Arzu Javadova
The problems deal with the natural conditions, biota and sediments of the South Caspian within Lankaran–Talish–Deniz and Khazar offshore areas, as well as anthropogenic impact on the ecological system of this region were discussed.
A.J.On ecology issue of South Caspian Lankaran–Talish–Deniz and Khazar areas.pdf
A.J.On ecology issue of South Caspian Lankaran–Talish–Deniz and Khazar areas.pdf
Dr. Arzu Javadova
Neogene ostracods from Paratethys are, potentially, a powerful biostratigraphic tool to depict the geological history of different basins [Styrian, Vienna, Pannonian, Dacian, Euxinic (former extent of the modern Black Sea basin), and Caspian-Aralic basins]. Yet, most species were described by different authors (Reuss, Méhes, Zalănyi, Livental) in mid-19th and early 20th centuries and, often, descriptions and illustrations are very poor. Very likely, the Neogene Paratethyan biodiversity is overestimated due to lack of literature exchange at time or the undervaluation of ecophenotypical intra-specific variability. As a consequence, often, under different specific (or even generic) names could be hidden the same species. Unfortunately, most of the historical ostracod collection are gone lost or destroyed and the only way to solve this problem is to get new samples from the type localities. Recently, clays and silts cropping out at Babazanan (Azerbaijan), type locality of the species described by Livental in 1929, were re-sampled, and here we present the results of our taxonomical studies of the collected ostracods providing new definition of the specific characters, mainly based on SEM illustration. An updated synonymy, paleogeographic and stratigraphic distribution starting from the extant literature, will be also provided.
Taxonomic harmonization of Paratethyan brackish ostracods described by Livent...
Taxonomic harmonization of Paratethyan brackish ostracods described by Livent...
Dr. Arzu Javadova
Recommandé
The new Government is targeting reforms and developments to radically transform the Iranian economy. Reforms are focused on: Better relationships with regional partners and the West Attracting foreign investment into the country Sustainable development of the petroleum sector: o Key for economic growth and welfare o Gradual removal of subsidies on energy Addressing and reduce unemployment Tightening fiscal policy to help the Central Bank with inflation Restructuring institutional decision making Stabilizing the Rial
Provinces of iran
Provinces of iran
Dr. Arzu Javadova
Using different public and private sources given field size distribution of Kurdsitan Iraq
Field size distribution of Kurdistan pptx
Field size distribution of Kurdistan pptx
Dr. Arzu Javadova
Reservoir modeling work flow chart
Reservoir modeling work flow chart
Reservoir modeling work flow chart
Dr. Arzu Javadova
The South Caspian Basin has many confirmed structures. It includes the offshore continuation of several major anticline trends extending from onshore side. The Umid Babek structure is one of the deepest structures of the Baku archipelago. It is strongly dislocated tectonically and is complicated by mud diapirism. Interpretation of 2D seismic data made it possible to determine the calculations for the area and depth in the Umid and Babek structures. The structures of Shah Deniz and Umid Babek are similar in terms of the history of their structural growth. Umid-Babek occupies the most advantageous position on the path of fluid migration from deep zones of depression and has favourable conditions for the accumulation and preservation of hydrocarbon deposits. U
РЕГИОНАЛЬНАЯ ГЕОЛОГИЯ_2021_3_испр финал1-10.pdf
РЕГИОНАЛЬНАЯ ГЕОЛОГИЯ_2021_3_испр финал1-10.pdf
Dr. Arzu Javadova
The results of reconnaissance studies within the Shakal and Halabja exploration blocks in Kurdistan are presented. Experimental studies were carried out using a mobile direct-prospecting technology, including modified methods of frequency-resonance processing and decoding of satellite images and photo images, vertical electric resonance scanning of the cross-section and a method of integral assessment of the oil and gas potential of large prospecting blocks and license areas. At the local survey site within the Shakal block, responses from oil, condensate, phosphorus and limestone were recorded. The lower boundary of the limestones was established at a depth of 4676 m. By scanning the cross-section from 2770 m, step 1 cm, the responses of oil from limestones were obtained from the intervals: 1) 2771-2794 m, 2) 2795.3-2815.45 m, 3) 2834.40-2854 m. During processing the image of the entire Halabja block, signals were recorded at the frequencies of oil, condensate, phosphorus gas, bacteria, sodium chloride and dolomite. At the 57 km hydrocarbon synthesis boundary, responses from oil, condensate and gas were recorded. When scanning the cross-section from 480 m to 4 km, step 50 cm, responses from oil were obtained from two intervals: 1) 1140-1200 m, and 2) 3310-3340 m. Within the local fragment of the block by scanning up to 5 km with a step of 1 m responses of oil from salt were recorded from the intervals: 1) 295-350 m, 2) 1190-1260 m, 3) 2015-2320 m). The response intervals within the 1st and 3rd horizons have been refined by scanning with a step of 5 cm. The results of experimental studies show that practical application of direct-prospecting methods and technologies will accelerate and optimize the exploration process for oil and gas.
RESULTS OF THE APPLICATION OF DIRECT-PROSPECTING TECHNOLOGY OF SATELLITE IMAG...
RESULTS OF THE APPLICATION OF DIRECT-PROSPECTING TECHNOLOGY OF SATELLITE IMAG...
Dr. Arzu Javadova
The results of the application of mobile direct-prospecting technology of frequency-resonance processing and interpretation of satellite images and photographs at the sites of hydrogen production, drilling wells, as well as within areas of hydrogen degassing in various regions are presented. Experimental reconnaissance studies were carried out to study the features of the deep structure of the hydrogen degassing areas. The developed mobile and low-cost technology include modified methods of satellite images and photo-images frequency-resonance processing and decoding, vertical electric-resonance scanning of a cross-section, as well as a method of integrated assessment of oil and gas potential of large prospecting blocks and license areas. Separate methods of direct-prospecting technology are based on the principles of the “substance” paradigm of geophysical research, the essence of which is searching for a specific substance - oil, gas, gas condensate, etc. The materials of instrumental measurements indicate that in regions of basalt volcano's location with roots at different depths, signals at hydrogen frequencies are almost always recorded. When scanning the cross-section, responses from hydrogen are recorded from the upper edges of basaltic volcanoes to their roots. It can be assumed that basaltic volcanoes are a kind of channel through which hydrogen migrates to the upper horizons of the cross-section and further into the atmosphere. Within many basaltic volcanoes at a depth of 68 km, deep (living) water is synthesized. Hydrogen-rich water is curative and can be used for wellness purposes. All surveyed zones of longevity on Earth are located within basalt volcanoes, in which water synthesized at a depth of 68 km migrates to the surface and is used for water supply. Hydrogen deposits can be formed by basaltic volcanoes in adjacent sealed reservoirs. Within some survey areas, responses at hydrogen frequencies from limestones, dolomites, and marls were recorded at shallow depths. Hydrogen deposits formed near basalt volcanoes in different types of reservoirs can be discovered and localized during areal exploration using proven methods. Direct-prospecting technology can also be used to study reservoirs in crystalline rocks (basalts including). Detailed studies and wells drilling in promising areas can be planned and carried out for hydrogen and living water at the same time. The result of the investigation indicates the advisability of using direct-prospecting methods of frequency-resonance processing of satellite images to detect zones of hydrogen accumulation in areas of basalt volcanoes location, as well as in areas of hydrogen degassing. The use of mobile and low-cost technology will significantly speed up the exploration process for hydrogen, as well as reduce the financial costs for its implementation.
Presentation1 final shortened.pdf
Presentation1 final shortened.pdf
Dr. Arzu Javadova
The problems deal with the natural conditions, biota and sediments of the South Caspian within Lankaran–Talish–Deniz and Khazar offshore areas, as well as anthropogenic impact on the ecological system of this region were discussed.
A.J.On ecology issue of South Caspian Lankaran–Talish–Deniz and Khazar areas.pdf
A.J.On ecology issue of South Caspian Lankaran–Talish–Deniz and Khazar areas.pdf
Dr. Arzu Javadova
Neogene ostracods from Paratethys are, potentially, a powerful biostratigraphic tool to depict the geological history of different basins [Styrian, Vienna, Pannonian, Dacian, Euxinic (former extent of the modern Black Sea basin), and Caspian-Aralic basins]. Yet, most species were described by different authors (Reuss, Méhes, Zalănyi, Livental) in mid-19th and early 20th centuries and, often, descriptions and illustrations are very poor. Very likely, the Neogene Paratethyan biodiversity is overestimated due to lack of literature exchange at time or the undervaluation of ecophenotypical intra-specific variability. As a consequence, often, under different specific (or even generic) names could be hidden the same species. Unfortunately, most of the historical ostracod collection are gone lost or destroyed and the only way to solve this problem is to get new samples from the type localities. Recently, clays and silts cropping out at Babazanan (Azerbaijan), type locality of the species described by Livental in 1929, were re-sampled, and here we present the results of our taxonomical studies of the collected ostracods providing new definition of the specific characters, mainly based on SEM illustration. An updated synonymy, paleogeographic and stratigraphic distribution starting from the extant literature, will be also provided.
Taxonomic harmonization of Paratethyan brackish ostracods described by Livent...
Taxonomic harmonization of Paratethyan brackish ostracods described by Livent...
Dr. Arzu Javadova
Comprehensive geological, geophysical study, and exploration drilling resulted in the vast material that makes it possible to assess microfauna content of South Caspian Basin. Commercial reservoirs have been established in the Miocene in the South Caspian Basin. The Miocene deposits in South Caspian Basin are of great practical and scientific interest as they underlie the formations of the thick Pliocene Productive series. The core samples taken from exploration wells of the Miocene deposits, where were recovered otholitite, abundant ostracod and foraminifera fauna. The studied sections allowed to define the detailed stratigraphy sequences into individual stratigraphic units: Pontian, Sarmatian, Conkian-Karaganian, Chokrakian, Maikopian deposits The facies of the Miocene deposits in the South Caspian offshore part of Basin vary considerably and these different facial sedimentary environments affected the microfauna composition as well. This is confirmed by rather abrupt changes in microfauna features from different regions of South Caspian Basin. The Miocene deposits of South Caspian offshore part of basin is rich in microfauna and many of ostracod species here were common in the Tethys and Paratethys bioprovince and is known as brackish and shallow marine genus in the ecology of ostracod assemblages
Microfauna of the Miocene Deposits in South Caspian_final versionof PRESENTAT...
Microfauna of the Miocene Deposits in South Caspian_final versionof PRESENTAT...
Dr. Arzu Javadova
For the geological and geophysical assessment of the South Caspian offshore Kapaz structure, seismic data were used with the construction of several structural maps. Four seismic horizons have been mapped: the top Pereriva, top Balakhany, top Surakhany suits, and top Akchagyl stage. The results of three wells drilled in the past were analyzed, the well- logs were correlated with neighboring exploration wells. Interpretation of seismic data shows that the Kapaz structure is located on the border of the sedimentary sources of the paleo Volga and paleo Amudarya. Regional seismic indicates that the paleo Volga probably continued to be the main source of terrigenous deposits. However, the Paleo-Amu Darya became a more important source of sediments during the Apsheron time. This is evidenced by the presence of clinoforms in seismic profiles direction, which is shown from the shelf margin in the dip direction to the west and southwest direction. It is shown that the Paleo-Amu Darya system eventually overlapped and pushed on the margin of the paleo-Volga shelf, effectively sealing the underlying terrigenous reservoir rocks. Growing diapir folds and compartmentation (southern and northern flank) were also observed in the feature of the structure. The reserves' calculation was carried out for each block of the Kapaz structure in scenarios P90, P50 and P10
Javadova Dr.A. Geological and geophysical assessment of the south caspian off...
Javadova Dr.A. Geological and geophysical assessment of the south caspian off...
Dr. Arzu Javadova
The results of a reconnaissance survey of a seismic profile on Ukraine territory are presented. Experimental studies were carried out with the aim of additional approbation of direct-prospecting methods and improvement of methodological techniques of their application in the exploration process for oil, gas and natural hydrogen, as well as in the study of the deep structural elements of the Earth. The results indicate that it is promising for the detection of HC deposits in the cross-section and the expediency of carrying out prospecting works of a detailed nature within it. In the northern part of the research area, by instrumental measurements a basalt volcanic complex has been localized, which is promising for of natural hydrogen and living water accumulations searching in the cross-section. During the cross-section scanning, responses at gas frequencies were recorded without interruption up to 5 km, which may indicate the presence of a deep channel within the surveyed area, through which oil, condensate and gas migrate to the upper horizons of the cross-section. The results of the survey indicate the advisability of direct-prospecting methods and technologies using when studying the deep structure of small areas and large blocks by geoelectric and seismic methods.
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdf
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdf
Dr. Arzu Javadova
Within the framework of a new, "substance" (“matter”) paradigm of geophysical research, a "direct" search for a specific physical substance is carried out: gas, oil, gas hydrates, water, ore minerals and rocks (gold, platinum, silver, zinc, uranium, diamonds, kimberlites, etc.). The initial stage in the development of this paradigm can be considered the first research and development on the "direct" methods for oil and gas searching.
Direct-prospecting methods_Presentation.ppt
Direct-prospecting methods_Presentation.ppt
Dr. Arzu Javadova
В рамках новой, «вещественной» парадигмы геофизических исследований осуществляется «прямой» поиск конкретного физического вещества: газа, нефти, газогидратов, воды, рудных полезных ископаемых и горных пород (золота, платина, серебро, цинк, уран, алмазы, кимберлиты и др.).
Прямопоисковая мобильная технология разведки на русском.ppt
Прямопоисковая мобильная технология разведки на русском.ppt
Dr. Arzu Javadova
Thus, the analysis of the borehole data, seismic data, and biostratigraphy confirmed that the Tertiary sediments consist of fluvial- deltaic–lacustrine sediments deposited in the isolated South Caspian Basin, particularly in the study area by several river systems. The study area has several characteristics typical of landlocked marine environments: Low salinity; low HD conditions, causing stratification of the water column. High primary productivity of the water mass, generating conditions of dissolved oxygen supersaturation and deficits (of phosphorus and probably of oxygen at night). Also at the sediment level, the heterogeneity of the substrate and low benthic fauna content is typical of confined habitats, in which environmental conditions are especially difficult for the higher organisms. The micro-pollutant concentration in both the water and sediment, a point also common to most confined habitats and related to the inflow from the catchment area. It is related to the fine fraction of the sediment and may be masked by the presence of numerous shell debris which “dilute” the muds and thereby the micro-pollutants and organic matter, usually settled on these fine sediment fractions. All the observations made on the study, substantial primary production, a paucity of benthos, etc are consistent with those made by different authors describing the Caspian Sea. The study area has high quantities of contaminants and low capabilities for dispersing potential intake, but on the other hand, has a distinct resistance to the influence of any future impediments
A.j.on ecology issue of south caspian lankaran–talish–deniz and khazar areas
A.j.on ecology issue of south caspian lankaran–talish–deniz and khazar areas
Dr. Arzu Javadova
Kapaz field is located in the central part of the Apsheron-Pribalkhan threshold between the Azeri and Livano structures- in the west of the Caspian sea. Water depth changes from 90 m in the east to 130 m in the west, in the area. In the seismic cross-sections of the Kapaz field, deposits from Quaternary to Miocene are observed, the cross-sections were revised using the Ostracoda and Formaninifera fauna contents based on regional well correlations. The tectonic structures are an asymmetric anticline striking NW-SE. The folding undulated the upper Pliocene twice and the middle Pliocene thrice. Secondary undulations present as dome-shaped uplifts (3-5 1.5-2,0 km). The size on the fold in the base of the upper division of the middle Pliocene is 25 x2.5 km. The structure in the base of the upper division of the Middle Pliocene is displaced relative to the structure of the top of the mIddle Pliocene to the northwest along the fol axis 3.5-4 km. Oil and gas potential in the southwestern and northeastern slopes of the structure is associated with the deposits from the suite of Pereriva and also with the underlying suits of PS. Concerning Kapaz field evaluation, it is recommended to drill wells to strip up to the KaS as it was done in the Turkmenistan sector of the Caspian Sea in the Livanova, Gubkina, and Lam field. Taking into account the anomalous high-pressure layer below the suite of Pereriva every effort should be taken to strip up to the KaS successfully
Geological & Prospective peculiarity of Kapaz field on South Caspian basin,
Geological & Prospective peculiarity of Kapaz field on South Caspian basin,
Dr. Arzu Javadova
The SW part of south Caspian offshore studied very poorly. Data studied from numerous offshore shallow engineering and deep exploration wells have provided useful information on the geology of the Tertiary- Quaternary sediments. The log, seismic data, and biostratigraphy confirmed that the Tertiary sediments consist of fluvial- deltaic–lacustrine sediments deposited in the isolated South Caspian Basin, particularly in the study area by several river systems. A Quarternary period is characterized by brackish water sediments. The "short" series of marine sediments of the deep and shallow facies of open sea bays, delta, and marine shallow waters are typical for the SW part of the Caspian. Pliocene and Quaternary sediments unconformably overlie more ancient formations, until the Mesozoic sediments are located at a relatively shallow depth. In the Lankaran-Talysh Deniz, the Miocene sequences below the middle part of Pliocene Pereryva formation are pinching out against the basin margin. The thickness of these series increases stepwise across the main structures giving evidence of a rift-system developing at the beginning of major subsidence in the South Caspian during the early Tertiary. No hydrocarbon discovery except little oil and gas shows are found in SW of the Caspian due to several geological reasons such as a reservoir, vertical and lateral migration problem.
To the geology of tertiary quaternary sediments of south-west part of the ...
To the geology of tertiary quaternary sediments of south-west part of the ...
Dr. Arzu Javadova
poster about coring procedure for training
2d poster about coring procedure
2d poster about coring procedure
Dr. Arzu Javadova
poster for training
1st poster example of core analysis program
1st poster example of core analysis program
Dr. Arzu Javadova
3d day of training
Days 3d porosity , permeability, fluid saturation
Days 3d porosity , permeability, fluid saturation
Dr. Arzu Javadova
2d day of training
Day 2 d coring & core analysis and reservoir geology
Day 2 d coring & core analysis and reservoir geology
Dr. Arzu Javadova
1st day of training
Core analysis & wellsite core acquisition, handling and transportation
Core analysis & wellsite core acquisition, handling and transportation
Dr. Arzu Javadova
Workshop presentation about shallow water Apsheron trend based on old seismic data
South Caspian shallow water Apsheron rend Geology
South Caspian shallow water Apsheron rend Geology
Dr. Arzu Javadova
Poster presentation for Kazan russian conference.24 29.09.2018 Нами были изучены остракоды из пробуренных скважин северного и центрального Бакинского архипелага: Бахар, Бахар-2, Шах дениз, Аран дениз, Себаил, Ленкоран дениз, Курдаши, Инам, Песчаний и др. Каспийского моря, что позволило коррелировать состав остракодовой фауны четвертичных отложений (рис. 1). В нашем распоряжении было свыше 350 образцов, около 100 видов Leptocythere и Loxoconcha. В целом, выделенный нами состав остракод Южного Каспия позволяет расчленить четвертичные отложения на новокаспийский, хвалынский, хазарский, бакинский и апшеронский надгоризонты с соответствующими горизонтами и слоями (рис. 2). Характерный комплекс постплиоценовой фауны остракод хорошо коррелируется с прибрежными разрезами Апшеронского полуострова: Песчаный, Алят, Локбатан, Пирсагат, Нефтчала. При определении видового состава использовались СЭМ фотографии остракод, собранных нами из скважин Апшеронского и Бакинского архипелагов
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...
Dr. Arzu Javadova
his paper presents the Microbial Prospection for Oil and Gas (MPOG) method, which uses microbiological techniques to explore for oil and gas. These techniques are based on the principle that light hydrocarbons from oil and gas fields escape to the earth’s surface, and this increased hydrocarbon supply above the fields creates conditions favorable for the development of highly specialized bacterial populations that feed on the hydrocarbons. This leads to significant increases in the microbial cell numbers and cell activity of these specialized microbes. By developing methods to establish the separate activities of methane-oxidizing bacteria (a gas indicator) and those bacteria that oxidize only ethane and higher hydrocarbons (oil indicators), it is possible to differentiate between oil fields with and without a free gas cap, and gas fields.In unexplored areas, MPOG represents a cost-effective method for preliminary exploration work. In mature areas, the method is helpful for ranking seismically defined geologic structures by indicating possible infill locations, as a contribution to reservoir characterization. No geologic or seismic data are required to carry out microbial prospection. In areas that have not yet been investigated geophysically, this technique can be applied as wildcat prospection. The sampling points are laid over the surface to be investigated, in the form of a map grid. The biochemical activity of the HCO represents the cumulative parameters. These are calculated by • quantifying the consumption of added hydrocarbons (methane and/or propane and butane) using gas chromatography and pressure measurements • determining the biological CO2 formation rate Microbial enhanced oil recovery (MEOR) represents the use of microorganisms to extract the remaining oil from reservoirs. This technique has the potential to be cost-efficient in the extraction of oil remained trapped in capillary pores of the formation rock or in areas not swept by the classical or modern enhanced oil recovery (EOR) methods, such as combustion, steams, miscible displacement, caustic surfactant-polymers flooding, etc. Thus, MEOR was developed as an alternative method for the secondary and tertiary extraction of oil from reservoirs,
Presentation mpog meor new
Presentation mpog meor new
Dr. Arzu Javadova
The South Caspian is one of the largest oil-producing regions within the Caspian Sea. Most of the offshore fields are focused here along with the main geologic oil and gas reserves of Azerbaijan. The development of the discovered fields, prospects and exploration of new ones require detailed study of the Quaternary deposits: their material composition, stratigraphy, thicknesses and other properties. It is necessary to study these issues not only for improvement of the efficiency, provide safe geological prospecting and exploration, but also to solve engineering and geological tasks related to the planned development of discovered oil and gas fields. Study of fauna and stratigraphy of the Quaternary deposits in the South Caspian is important to learn the Quaternary history of the Caspian Sea. The Quaternary time is known for its frequent and abrupt fluctuations in climate, ocean and sea levels, considerable changes in topography, fauna, flora and other natural components of the Earth. The large-scale well drilling in the South Caspian water area provided geological information particularly about ostracod fauna, stratigraphy and litho-facies features of the Quaternary deposits of the studied regions. We investigated the systematic composition and distribution regularities of ostracod fauna from the Quaternary deposits over the vast South Caspian territory, including the stratigraphic role of the fauna and correlation of the data with the coastal –onshore area. Multiple well sections and their enclosed micro- and macro fauna were the study target. When we analyzed and correlated well sections and natural outcrops we used other methods like lithological, macro fauna, radiometric, electric logging, seismic logging as well. The result of our study allowed us to design a detailed stratigraphic chart for the Quaternary deposits of the entire South Caspian basin. For the first time the Quaternary deposits of the South Caspian breakdown with 5 supra horizons, 10 horizons with 7 index species. Index species were identified on the successive change of zonal complexes- biozones. All these subdivisions play a regional role and correlated well with the ones from the adjacent areas of the Caspian region. The paleontological processing of individual ostracod of genera: Leptocythere, Amniocythere, Euxinocythere, others allowed us to identify specific features among them in order to differentiate a new ostracod species. We also highlighted the issues of stratigraphy, facies analysis and thicknesses of the Quaternary deposits in the South Caspian. The analysis of facies, thicknesses and fauna distribution shows that in the Quaternary time the South Caspian region was characterized by rather dynamic paleogeographic settings: along with the active change of the sea bottom topography, salinity and temperature varied considerably and often, as well as the sea level.
The Quaternary deposits of the South Caspian and the adjacent areas on ostrac...
The Quaternary deposits of the South Caspian and the adjacent areas on ostrac...
Dr. Arzu Javadova
This presentation published in international Earth Sciences Colloquium of the Aegean Regions, in Izmir, Turkey in 2005. The Apsheron trend characterised by large, east to west striking folds and structures of the Pliocene section overlying and burying the underlying rifted margin structures and half-grabens of the Cretaceous, Jurassic and possibly Triassic continental margin and shelf. The Tertiary structures display strike-slip influence, such as reversal of normal faults that bound the underlying half grabens; local back thrusting and flower-like structuring are common. The most significant volumetric potential lies in the offshore. Three elements are key to the extraordinary oil and gas potential of the South Caspian Basin. The high-quality reservoir sands are the Volga Pliocene delta and a lesser extent.
Geological &prospective peculiarity of Kapaz field on S.Caspian part 29 36
Geological &prospective peculiarity of Kapaz field on S.Caspian part 29 36
Dr. Arzu Javadova
This presentation published in international Earth Sciences Colloquium of the Aegean Regions, in Izmir, Turkey in 2005.S.Caspian basin is prominent basin with thick MZ-GZ terrigenous depositional fill encompassed by Alpine fold belt. The S. Caspian deep and basin proper is probably remnant oceanic crust of the Neo Thethys caught (пойманный) between the Jurassic Сretaceous carbonate platform and continental margin in the north accreted islands arc terrаin and Gondwana in the south. S. Capsian basin borders with prominent folt system of Major Caucasus & Copetdag on the north which are linked together across the basin via Apsheron-Pre Balkhan uplift belt which consists of 2 anticline lines: Apsheron-Turkmenbashy and Apsheron-Cheleken one
Geological &prospective peculiarity of Kapaz field on S.Caspian part 19 27
Geological &prospective peculiarity of Kapaz field on S.Caspian part 19 27
Dr. Arzu Javadova
This presentation published in international Earth Sciences Colloquium of the Aegean Regions, in Izmir, Turkey in 2005. The Kapaz structure was initially called Promezhutochnoye and later dubbed Oktyabr'skaya Revolyutsiya. Field Kapaz located in the central part of the Apsheron-Pribalkhan threshold between the fields Azeri and Livanov-West in Caspian sea. Water depth variations change from 90m in the east, up to 130m in the west Seismic survey CDP determined the structure in 1981. In addition to the Productive Sequence, main reservoirs have been proven in carbonates and volcanic sands of Cretaceous age and the Oligo-Miocene Maikop Series. These reservoirs are of poorer quality than the Productive Sequence and are consequently more challenging to commercial development. The petroleum geology of Azerbaijan dominated by a single sedimentary basin - the South Caspian Basin
Geological & prospective peculiarity of Kapaz field on S.Caspian part 1 9
Geological & prospective peculiarity of Kapaz field on S.Caspian part 1 9
Dr. Arzu Javadova
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Plus de Dr. Arzu Javadova
Comprehensive geological, geophysical study, and exploration drilling resulted in the vast material that makes it possible to assess microfauna content of South Caspian Basin. Commercial reservoirs have been established in the Miocene in the South Caspian Basin. The Miocene deposits in South Caspian Basin are of great practical and scientific interest as they underlie the formations of the thick Pliocene Productive series. The core samples taken from exploration wells of the Miocene deposits, where were recovered otholitite, abundant ostracod and foraminifera fauna. The studied sections allowed to define the detailed stratigraphy sequences into individual stratigraphic units: Pontian, Sarmatian, Conkian-Karaganian, Chokrakian, Maikopian deposits The facies of the Miocene deposits in the South Caspian offshore part of Basin vary considerably and these different facial sedimentary environments affected the microfauna composition as well. This is confirmed by rather abrupt changes in microfauna features from different regions of South Caspian Basin. The Miocene deposits of South Caspian offshore part of basin is rich in microfauna and many of ostracod species here were common in the Tethys and Paratethys bioprovince and is known as brackish and shallow marine genus in the ecology of ostracod assemblages
Microfauna of the Miocene Deposits in South Caspian_final versionof PRESENTAT...
Microfauna of the Miocene Deposits in South Caspian_final versionof PRESENTAT...
Dr. Arzu Javadova
For the geological and geophysical assessment of the South Caspian offshore Kapaz structure, seismic data were used with the construction of several structural maps. Four seismic horizons have been mapped: the top Pereriva, top Balakhany, top Surakhany suits, and top Akchagyl stage. The results of three wells drilled in the past were analyzed, the well- logs were correlated with neighboring exploration wells. Interpretation of seismic data shows that the Kapaz structure is located on the border of the sedimentary sources of the paleo Volga and paleo Amudarya. Regional seismic indicates that the paleo Volga probably continued to be the main source of terrigenous deposits. However, the Paleo-Amu Darya became a more important source of sediments during the Apsheron time. This is evidenced by the presence of clinoforms in seismic profiles direction, which is shown from the shelf margin in the dip direction to the west and southwest direction. It is shown that the Paleo-Amu Darya system eventually overlapped and pushed on the margin of the paleo-Volga shelf, effectively sealing the underlying terrigenous reservoir rocks. Growing diapir folds and compartmentation (southern and northern flank) were also observed in the feature of the structure. The reserves' calculation was carried out for each block of the Kapaz structure in scenarios P90, P50 and P10
Javadova Dr.A. Geological and geophysical assessment of the south caspian off...
Javadova Dr.A. Geological and geophysical assessment of the south caspian off...
Dr. Arzu Javadova
The results of a reconnaissance survey of a seismic profile on Ukraine territory are presented. Experimental studies were carried out with the aim of additional approbation of direct-prospecting methods and improvement of methodological techniques of their application in the exploration process for oil, gas and natural hydrogen, as well as in the study of the deep structural elements of the Earth. The results indicate that it is promising for the detection of HC deposits in the cross-section and the expediency of carrying out prospecting works of a detailed nature within it. In the northern part of the research area, by instrumental measurements a basalt volcanic complex has been localized, which is promising for of natural hydrogen and living water accumulations searching in the cross-section. During the cross-section scanning, responses at gas frequencies were recorded without interruption up to 5 km, which may indicate the presence of a deep channel within the surveyed area, through which oil, condensate and gas migrate to the upper horizons of the cross-section. The results of the survey indicate the advisability of direct-prospecting methods and technologies using when studying the deep structure of small areas and large blocks by geoelectric and seismic methods.
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdf
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdf
Dr. Arzu Javadova
Within the framework of a new, "substance" (“matter”) paradigm of geophysical research, a "direct" search for a specific physical substance is carried out: gas, oil, gas hydrates, water, ore minerals and rocks (gold, platinum, silver, zinc, uranium, diamonds, kimberlites, etc.). The initial stage in the development of this paradigm can be considered the first research and development on the "direct" methods for oil and gas searching.
Direct-prospecting methods_Presentation.ppt
Direct-prospecting methods_Presentation.ppt
Dr. Arzu Javadova
В рамках новой, «вещественной» парадигмы геофизических исследований осуществляется «прямой» поиск конкретного физического вещества: газа, нефти, газогидратов, воды, рудных полезных ископаемых и горных пород (золота, платина, серебро, цинк, уран, алмазы, кимберлиты и др.).
Прямопоисковая мобильная технология разведки на русском.ppt
Прямопоисковая мобильная технология разведки на русском.ppt
Dr. Arzu Javadova
Thus, the analysis of the borehole data, seismic data, and biostratigraphy confirmed that the Tertiary sediments consist of fluvial- deltaic–lacustrine sediments deposited in the isolated South Caspian Basin, particularly in the study area by several river systems. The study area has several characteristics typical of landlocked marine environments: Low salinity; low HD conditions, causing stratification of the water column. High primary productivity of the water mass, generating conditions of dissolved oxygen supersaturation and deficits (of phosphorus and probably of oxygen at night). Also at the sediment level, the heterogeneity of the substrate and low benthic fauna content is typical of confined habitats, in which environmental conditions are especially difficult for the higher organisms. The micro-pollutant concentration in both the water and sediment, a point also common to most confined habitats and related to the inflow from the catchment area. It is related to the fine fraction of the sediment and may be masked by the presence of numerous shell debris which “dilute” the muds and thereby the micro-pollutants and organic matter, usually settled on these fine sediment fractions. All the observations made on the study, substantial primary production, a paucity of benthos, etc are consistent with those made by different authors describing the Caspian Sea. The study area has high quantities of contaminants and low capabilities for dispersing potential intake, but on the other hand, has a distinct resistance to the influence of any future impediments
A.j.on ecology issue of south caspian lankaran–talish–deniz and khazar areas
A.j.on ecology issue of south caspian lankaran–talish–deniz and khazar areas
Dr. Arzu Javadova
Kapaz field is located in the central part of the Apsheron-Pribalkhan threshold between the Azeri and Livano structures- in the west of the Caspian sea. Water depth changes from 90 m in the east to 130 m in the west, in the area. In the seismic cross-sections of the Kapaz field, deposits from Quaternary to Miocene are observed, the cross-sections were revised using the Ostracoda and Formaninifera fauna contents based on regional well correlations. The tectonic structures are an asymmetric anticline striking NW-SE. The folding undulated the upper Pliocene twice and the middle Pliocene thrice. Secondary undulations present as dome-shaped uplifts (3-5 1.5-2,0 km). The size on the fold in the base of the upper division of the middle Pliocene is 25 x2.5 km. The structure in the base of the upper division of the Middle Pliocene is displaced relative to the structure of the top of the mIddle Pliocene to the northwest along the fol axis 3.5-4 km. Oil and gas potential in the southwestern and northeastern slopes of the structure is associated with the deposits from the suite of Pereriva and also with the underlying suits of PS. Concerning Kapaz field evaluation, it is recommended to drill wells to strip up to the KaS as it was done in the Turkmenistan sector of the Caspian Sea in the Livanova, Gubkina, and Lam field. Taking into account the anomalous high-pressure layer below the suite of Pereriva every effort should be taken to strip up to the KaS successfully
Geological & Prospective peculiarity of Kapaz field on South Caspian basin,
Geological & Prospective peculiarity of Kapaz field on South Caspian basin,
Dr. Arzu Javadova
The SW part of south Caspian offshore studied very poorly. Data studied from numerous offshore shallow engineering and deep exploration wells have provided useful information on the geology of the Tertiary- Quaternary sediments. The log, seismic data, and biostratigraphy confirmed that the Tertiary sediments consist of fluvial- deltaic–lacustrine sediments deposited in the isolated South Caspian Basin, particularly in the study area by several river systems. A Quarternary period is characterized by brackish water sediments. The "short" series of marine sediments of the deep and shallow facies of open sea bays, delta, and marine shallow waters are typical for the SW part of the Caspian. Pliocene and Quaternary sediments unconformably overlie more ancient formations, until the Mesozoic sediments are located at a relatively shallow depth. In the Lankaran-Talysh Deniz, the Miocene sequences below the middle part of Pliocene Pereryva formation are pinching out against the basin margin. The thickness of these series increases stepwise across the main structures giving evidence of a rift-system developing at the beginning of major subsidence in the South Caspian during the early Tertiary. No hydrocarbon discovery except little oil and gas shows are found in SW of the Caspian due to several geological reasons such as a reservoir, vertical and lateral migration problem.
To the geology of tertiary quaternary sediments of south-west part of the ...
To the geology of tertiary quaternary sediments of south-west part of the ...
Dr. Arzu Javadova
poster about coring procedure for training
2d poster about coring procedure
2d poster about coring procedure
Dr. Arzu Javadova
poster for training
1st poster example of core analysis program
1st poster example of core analysis program
Dr. Arzu Javadova
3d day of training
Days 3d porosity , permeability, fluid saturation
Days 3d porosity , permeability, fluid saturation
Dr. Arzu Javadova
2d day of training
Day 2 d coring & core analysis and reservoir geology
Day 2 d coring & core analysis and reservoir geology
Dr. Arzu Javadova
1st day of training
Core analysis & wellsite core acquisition, handling and transportation
Core analysis & wellsite core acquisition, handling and transportation
Dr. Arzu Javadova
Workshop presentation about shallow water Apsheron trend based on old seismic data
South Caspian shallow water Apsheron rend Geology
South Caspian shallow water Apsheron rend Geology
Dr. Arzu Javadova
Poster presentation for Kazan russian conference.24 29.09.2018 Нами были изучены остракоды из пробуренных скважин северного и центрального Бакинского архипелага: Бахар, Бахар-2, Шах дениз, Аран дениз, Себаил, Ленкоран дениз, Курдаши, Инам, Песчаний и др. Каспийского моря, что позволило коррелировать состав остракодовой фауны четвертичных отложений (рис. 1). В нашем распоряжении было свыше 350 образцов, около 100 видов Leptocythere и Loxoconcha. В целом, выделенный нами состав остракод Южного Каспия позволяет расчленить четвертичные отложения на новокаспийский, хвалынский, хазарский, бакинский и апшеронский надгоризонты с соответствующими горизонтами и слоями (рис. 2). Характерный комплекс постплиоценовой фауны остракод хорошо коррелируется с прибрежными разрезами Апшеронского полуострова: Песчаный, Алят, Локбатан, Пирсагат, Нефтчала. При определении видового состава использовались СЭМ фотографии остракод, собранных нами из скважин Апшеронского и Бакинского архипелагов
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...
Dr. Arzu Javadova
his paper presents the Microbial Prospection for Oil and Gas (MPOG) method, which uses microbiological techniques to explore for oil and gas. These techniques are based on the principle that light hydrocarbons from oil and gas fields escape to the earth’s surface, and this increased hydrocarbon supply above the fields creates conditions favorable for the development of highly specialized bacterial populations that feed on the hydrocarbons. This leads to significant increases in the microbial cell numbers and cell activity of these specialized microbes. By developing methods to establish the separate activities of methane-oxidizing bacteria (a gas indicator) and those bacteria that oxidize only ethane and higher hydrocarbons (oil indicators), it is possible to differentiate between oil fields with and without a free gas cap, and gas fields.In unexplored areas, MPOG represents a cost-effective method for preliminary exploration work. In mature areas, the method is helpful for ranking seismically defined geologic structures by indicating possible infill locations, as a contribution to reservoir characterization. No geologic or seismic data are required to carry out microbial prospection. In areas that have not yet been investigated geophysically, this technique can be applied as wildcat prospection. The sampling points are laid over the surface to be investigated, in the form of a map grid. The biochemical activity of the HCO represents the cumulative parameters. These are calculated by • quantifying the consumption of added hydrocarbons (methane and/or propane and butane) using gas chromatography and pressure measurements • determining the biological CO2 formation rate Microbial enhanced oil recovery (MEOR) represents the use of microorganisms to extract the remaining oil from reservoirs. This technique has the potential to be cost-efficient in the extraction of oil remained trapped in capillary pores of the formation rock or in areas not swept by the classical or modern enhanced oil recovery (EOR) methods, such as combustion, steams, miscible displacement, caustic surfactant-polymers flooding, etc. Thus, MEOR was developed as an alternative method for the secondary and tertiary extraction of oil from reservoirs,
Presentation mpog meor new
Presentation mpog meor new
Dr. Arzu Javadova
The South Caspian is one of the largest oil-producing regions within the Caspian Sea. Most of the offshore fields are focused here along with the main geologic oil and gas reserves of Azerbaijan. The development of the discovered fields, prospects and exploration of new ones require detailed study of the Quaternary deposits: their material composition, stratigraphy, thicknesses and other properties. It is necessary to study these issues not only for improvement of the efficiency, provide safe geological prospecting and exploration, but also to solve engineering and geological tasks related to the planned development of discovered oil and gas fields. Study of fauna and stratigraphy of the Quaternary deposits in the South Caspian is important to learn the Quaternary history of the Caspian Sea. The Quaternary time is known for its frequent and abrupt fluctuations in climate, ocean and sea levels, considerable changes in topography, fauna, flora and other natural components of the Earth. The large-scale well drilling in the South Caspian water area provided geological information particularly about ostracod fauna, stratigraphy and litho-facies features of the Quaternary deposits of the studied regions. We investigated the systematic composition and distribution regularities of ostracod fauna from the Quaternary deposits over the vast South Caspian territory, including the stratigraphic role of the fauna and correlation of the data with the coastal –onshore area. Multiple well sections and their enclosed micro- and macro fauna were the study target. When we analyzed and correlated well sections and natural outcrops we used other methods like lithological, macro fauna, radiometric, electric logging, seismic logging as well. The result of our study allowed us to design a detailed stratigraphic chart for the Quaternary deposits of the entire South Caspian basin. For the first time the Quaternary deposits of the South Caspian breakdown with 5 supra horizons, 10 horizons with 7 index species. Index species were identified on the successive change of zonal complexes- biozones. All these subdivisions play a regional role and correlated well with the ones from the adjacent areas of the Caspian region. The paleontological processing of individual ostracod of genera: Leptocythere, Amniocythere, Euxinocythere, others allowed us to identify specific features among them in order to differentiate a new ostracod species. We also highlighted the issues of stratigraphy, facies analysis and thicknesses of the Quaternary deposits in the South Caspian. The analysis of facies, thicknesses and fauna distribution shows that in the Quaternary time the South Caspian region was characterized by rather dynamic paleogeographic settings: along with the active change of the sea bottom topography, salinity and temperature varied considerably and often, as well as the sea level.
The Quaternary deposits of the South Caspian and the adjacent areas on ostrac...
The Quaternary deposits of the South Caspian and the adjacent areas on ostrac...
Dr. Arzu Javadova
This presentation published in international Earth Sciences Colloquium of the Aegean Regions, in Izmir, Turkey in 2005. The Apsheron trend characterised by large, east to west striking folds and structures of the Pliocene section overlying and burying the underlying rifted margin structures and half-grabens of the Cretaceous, Jurassic and possibly Triassic continental margin and shelf. The Tertiary structures display strike-slip influence, such as reversal of normal faults that bound the underlying half grabens; local back thrusting and flower-like structuring are common. The most significant volumetric potential lies in the offshore. Three elements are key to the extraordinary oil and gas potential of the South Caspian Basin. The high-quality reservoir sands are the Volga Pliocene delta and a lesser extent.
Geological &prospective peculiarity of Kapaz field on S.Caspian part 29 36
Geological &prospective peculiarity of Kapaz field on S.Caspian part 29 36
Dr. Arzu Javadova
This presentation published in international Earth Sciences Colloquium of the Aegean Regions, in Izmir, Turkey in 2005.S.Caspian basin is prominent basin with thick MZ-GZ terrigenous depositional fill encompassed by Alpine fold belt. The S. Caspian deep and basin proper is probably remnant oceanic crust of the Neo Thethys caught (пойманный) between the Jurassic Сretaceous carbonate platform and continental margin in the north accreted islands arc terrаin and Gondwana in the south. S. Capsian basin borders with prominent folt system of Major Caucasus & Copetdag on the north which are linked together across the basin via Apsheron-Pre Balkhan uplift belt which consists of 2 anticline lines: Apsheron-Turkmenbashy and Apsheron-Cheleken one
Geological &prospective peculiarity of Kapaz field on S.Caspian part 19 27
Geological &prospective peculiarity of Kapaz field on S.Caspian part 19 27
Dr. Arzu Javadova
This presentation published in international Earth Sciences Colloquium of the Aegean Regions, in Izmir, Turkey in 2005. The Kapaz structure was initially called Promezhutochnoye and later dubbed Oktyabr'skaya Revolyutsiya. Field Kapaz located in the central part of the Apsheron-Pribalkhan threshold between the fields Azeri and Livanov-West in Caspian sea. Water depth variations change from 90m in the east, up to 130m in the west Seismic survey CDP determined the structure in 1981. In addition to the Productive Sequence, main reservoirs have been proven in carbonates and volcanic sands of Cretaceous age and the Oligo-Miocene Maikop Series. These reservoirs are of poorer quality than the Productive Sequence and are consequently more challenging to commercial development. The petroleum geology of Azerbaijan dominated by a single sedimentary basin - the South Caspian Basin
Geological & prospective peculiarity of Kapaz field on S.Caspian part 1 9
Geological & prospective peculiarity of Kapaz field on S.Caspian part 1 9
Dr. Arzu Javadova
Plus de Dr. Arzu Javadova
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Microfauna of the Miocene Deposits in South Caspian_final versionof PRESENTAT...
Microfauna of the Miocene Deposits in South Caspian_final versionof PRESENTAT...
Javadova Dr.A. Geological and geophysical assessment of the south caspian off...
Javadova Dr.A. Geological and geophysical assessment of the south caspian off...
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdf
Results of reconnaissance survey _Profile TESZ-2021_FINAL_short version.pdf
Direct-prospecting methods_Presentation.ppt
Direct-prospecting methods_Presentation.ppt
Прямопоисковая мобильная технология разведки на русском.ppt
Прямопоисковая мобильная технология разведки на русском.ppt
A.j.on ecology issue of south caspian lankaran–talish–deniz and khazar areas
A.j.on ecology issue of south caspian lankaran–talish–deniz and khazar areas
Geological & Prospective peculiarity of Kapaz field on South Caspian basin,
Geological & Prospective peculiarity of Kapaz field on South Caspian basin,
To the geology of tertiary quaternary sediments of south-west part of the ...
To the geology of tertiary quaternary sediments of south-west part of the ...
2d poster about coring procedure
2d poster about coring procedure
1st poster example of core analysis program
1st poster example of core analysis program
Days 3d porosity , permeability, fluid saturation
Days 3d porosity , permeability, fluid saturation
Day 2 d coring & core analysis and reservoir geology
Day 2 d coring & core analysis and reservoir geology
Core analysis & wellsite core acquisition, handling and transportation
Core analysis & wellsite core acquisition, handling and transportation
South Caspian shallow water Apsheron rend Geology
South Caspian shallow water Apsheron rend Geology
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...
STRATIGRAPHIC PECULARITIES OF OSTRACOD DISTRIBUTION IN BAKU ARCHIPELAGO, THE ...
Presentation mpog meor new
Presentation mpog meor new
The Quaternary deposits of the South Caspian and the adjacent areas on ostrac...
The Quaternary deposits of the South Caspian and the adjacent areas on ostrac...
Geological &prospective peculiarity of Kapaz field on S.Caspian part 29 36
Geological &prospective peculiarity of Kapaz field on S.Caspian part 29 36
Geological &prospective peculiarity of Kapaz field on S.Caspian part 19 27
Geological &prospective peculiarity of Kapaz field on S.Caspian part 19 27
Geological & prospective peculiarity of Kapaz field on S.Caspian part 1 9
Geological & prospective peculiarity of Kapaz field on S.Caspian part 1 9
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My music video presentation
My Presentation "In Your Hands" by Halle Bailey
My Presentation "In Your Hands" by Halle Bailey
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A training I conducted while I was the Technical Editor at Booth Management Consulting, LLC (BMC). The training educated my team on preventing common grammatical errors, Grammarly, Microsoft Word, Shared file environments, and my role as Technical Editor.
Report Writing Webinar Training
Report Writing Webinar Training
KylaCullinane
Presentation about poverty in France.
Causes of poverty in France presentation.pptx
Causes of poverty in France presentation.pptx
CamilleBoulbin1
The workplace ecosystem of the future. Green Building Summit, Bratislava 24.4.2024. Kasper Fabritius.
The workplace ecosystem of the future 24.4.2024 Fabritius_share ii.pdf
The workplace ecosystem of the future 24.4.2024 Fabritius_share ii.pdf
Senaatti-kiinteistöt
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AWS Data Engineer Associate (DEA-C01) Exam Dumps 2024.pdf
AWS Data Engineer Associate (DEA-C01) Exam Dumps 2024.pdf
SkillCertProExams
I had the honour of presenting my reflections on the autobiography of Professor Isaac Folorunso Adewole, titled "Uncommon Grace." As someone deeply invested in documentation and history, I found Professor Adewole's decision to narrate his journey from humble beginnings to occupying one of the highest offices in the land both inspiring and invaluable. In this eloquently written memoir, Professor Adewole provides a comprehensive account of his life, from his ancestral roots to his time as Minister of Health in Nigeria. The unique aspect of this autobiography is that he portrayed himself authentically without taking the help of third-party narratives, which is often seen in accounts of high-ranking officials. His upbringing was greatly influenced by his father's commitment to education. He became a prominent figure in advocating for the rights of the underprivileged through trade unionism. His story is one of unwavering determination, resilience, and faith. His experiences, including both successes and struggles, provide priceless lessons on leadership, perseverance, and the alignment of personal values with public service. While reading "Uncommon Grace," I was struck by the deep leadership lessons that are embedded within its chapters. Professor Adewole stresses the importance of inclusivity, servant leadership, and planning, which are all highly relevant in today's complex world. His commitment to accountability, as well as his primary responsibility as a researcher, serves as a guiding light for aspiring leaders across various disciplines. During his tenure as the Vice Chancellor of the University of Ibadan, he led with visionary leadership and transformative impact. His accomplishments have been meticulously documented in the book, which can serve as a blueprint for rejuvenating institutions and promoting academic excellence. In the latter part of his autobiography, Professor Adewole shares his experiences as a Minister, detailing the challenges he faced while serving the public with integrity and courage. His reflections on the complexities of public service, coupled with his commitment to the well-being of the nation, offer practical insights for policymakers and citizens alike. I have carefully read "Uncommon Grace" and it is more than just a memoir. It is a timeless book that is hard to put down once you start reading. While intellectuals may continue to debate whether uncommon grace was made possible by uncommon preparation or the other way around, I applaud Professor Adewole for sharing his ideas, knowledge, and experience with the public. I highly recommend this book to everyone.
Uncommon Grace The Autobiography of Isaac Folorunso
Uncommon Grace The Autobiography of Isaac Folorunso
Kayode Fayemi
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ICT role in 21st century education Role of ICT in education Is importance to you knowing
ICT role in 21st century education and it's challenges.pdf
ICT role in 21st century education and it's challenges.pdf
Islamia university of Rahim Yar khan campus
Music video treatment for Dreaming
Dreaming Music Video Treatment _ Project & Portfolio III
Dreaming Music Video Treatment _ Project & Portfolio III
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Compiled during the Project & Portfolio 3: Entertainment Business course at Full Sail University, this music video treatment outlines our team's creative ideas and was presented to the artist and producers.
Dreaming Marissa Sánchez Music Video Treatment
Dreaming Marissa Sánchez Music Video Treatment
nswingard
Yesterday in Lagos, I had the honour of delivering a lecture titled “If this Giant Must Walk; Manifesto for a New Nigeria“ at the Inaugural Memorial Lecture of Prince Emeka Obasi, founder and publisher of Business Hallmark and the inspirational figure behind the Public Policy Research and Analysis Centre - promoters of the revered Zik Leadership and Governance Awards. My lecture focused on the challenges of nation-building in Nigeria and how we can approach them in a way that promotes progress and unity. I discussed the many sources of concern about our country’s future prospects, including violent conflicts, revisionist contestations of the Amalgamation Act of 1914, discontent with the Nigerian economy, and dysfunctions in the federal system. Central to my lecture was the call to address these challenges by crafting a new manifesto for Nigeria. This manifesto, I proposed, should champion integrity, compassion, character, competence, and commitment to national unity and progress within a framework of democratic governance and cultural diversity. I firmly believe that by doing so, we can guide Nigeria to stride forward with pride and purpose. I want to thank the Board and Management of the Public Policy Forum for their kind invitation to speak at this important event and for their commitment to promoting public policy research and analysis in Nigeria. My gratitude also to the late Prince Emeka Obasi, a true inspiration and a builder of bridges across divides, for his contributions to the country. My thoughts are with his family and loved ones.
If this Giant Must Walk: A Manifesto for a New Nigeria
If this Giant Must Walk: A Manifesto for a New Nigeria
Kayode Fayemi
Beowulf
Chiulli_Aurora_Oman_Raffaele_Beowulf.pptx
Chiulli_Aurora_Oman_Raffaele_Beowulf.pptx
raffaeleoman
The slide from my talk at Drupalcamp Ghent 2024 about digital collaboration with Microsoft 365 and the Drupal CMS using the contributed module "Microsoft 365 connector"
Digital collaboration with Microsoft 365 as extension of Drupal
Digital collaboration with Microsoft 365 as extension of Drupal
Fabian de Rijk
10th class notes by MS. SAJIDA LODHI Pakistan studies Teacher Msc.Pakistan Studies. Bachelor degree in Eduction. TEFL DIP
lONG QUESTION ANSWER PAKISTAN STUDIES10.
lONG QUESTION ANSWER PAKISTAN STUDIES10.
lodhisaajjda
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My Presentation "In Your Hands" by Halle Bailey
My Presentation "In Your Hands" by Halle Bailey
Report Writing Webinar Training
Report Writing Webinar Training
Causes of poverty in France presentation.pptx
Causes of poverty in France presentation.pptx
The workplace ecosystem of the future 24.4.2024 Fabritius_share ii.pdf
The workplace ecosystem of the future 24.4.2024 Fabritius_share ii.pdf
AWS Data Engineer Associate (DEA-C01) Exam Dumps 2024.pdf
AWS Data Engineer Associate (DEA-C01) Exam Dumps 2024.pdf
Uncommon Grace The Autobiography of Isaac Folorunso
Uncommon Grace The Autobiography of Isaac Folorunso
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ICT role in 21st century education and it's challenges.pdf
ICT role in 21st century education and it's challenges.pdf
Dreaming Music Video Treatment _ Project & Portfolio III
Dreaming Music Video Treatment _ Project & Portfolio III
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Dreaming Marissa Sánchez Music Video Treatment
Dreaming Marissa Sánchez Music Video Treatment
If this Giant Must Walk: A Manifesto for a New Nigeria
If this Giant Must Walk: A Manifesto for a New Nigeria
Chiulli_Aurora_Oman_Raffaele_Beowulf.pptx
Chiulli_Aurora_Oman_Raffaele_Beowulf.pptx
Digital collaboration with Microsoft 365 as extension of Drupal
Digital collaboration with Microsoft 365 as extension of Drupal
lONG QUESTION ANSWER PAKISTAN STUDIES10.
lONG QUESTION ANSWER PAKISTAN STUDIES10.
Iran oil and gas infrastructure
1.
Iran oil and
gas infrastructure
2.
Regional existing and
planned gas pipelines
3.
Regional existing and
planned gas pipeline capacity and utilization (BCM for 2014; capacity in 2020 only for planned pipelines)
4.
0 50,000 100,000 150,000 200,000 250,000 2007 2008 2009
2010 2011 2012 Length(km) Gas distribution pipe
5.
Technical specifications for
pipelines (Photo courtesy: Reuters)
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