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Rocks of Singapore (2013)
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KYI KHIN
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Some collection of Singapore Rocks and thin sections photo-micrographs
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The Bengal-Arakan Neogene basin is one of the representative clastic basins formed in the frontal part of the Himalayan orogenic belt since late Cenozoic (Kyi Khin et al., 2014, 2017). The basin occupies the eastern part of Paleo-Bengal basin, the biggest basin of the world in Cenozoic. It is located at the unique tectonic setting; a juncture of the collision zone between the Indian and Asian continents to the north and the subduction zone between the Indian Plate and Myanmar Plate to the east. The purpose of the study is to shed some light on the sedimentation in the distal foreland basin of the Himalaya-Bengal System, related with control on timing and distribution of erosional fluxes derived from the uplifted Himalayas since Early Miocene. Chemical weathering strongly affects the major-element geochemistry and mineralogy of siliciclastic sediments. The predicted weathering trend line intersects the feldspar and shows the proportion of plagioclase and K-feldspar of the fresh rock between granodiorite and granite composition. The presentation will focus on the results of integrated study of sequence stratigraphy on the Miocene sediments and the provenance studies based on the petrography and chemical composition of sandstones and shales in order to interpret the weathering episode and relationship between tectonic denudation of Himalaya orogenic belts and reciprocal sedimentation related with foreland thrusting of Himalaya-Bengal System.
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The Japan Archipelago is a part of the Circum Pacific Orogenic Belt and is geologically very unstable. The bedrock materials which comprise the mountain terrain have been severely fractured since its formation and have developed numerous fault fracture zones. Furthermore, the islands are located within the monsoon zone and receive abundant rainfall. Coupled with early summer rainy spells and later typhoons, numerous landslides occur resulting in staggering damages. The geological and geographical situations attribute important factors in Landslide Evolution and Landslide Topography. Among the slopes that have landslide topography, there are many Static Landslides (Old Landslides) with erosional features and dissected scarps caused many active landslides. Main factors of the Landslide and slope failures triggered by Typhoon No. 14 are heavy rainfall (1,322mm) and geologic characteristics of the earth materials formed by highly deformed Pre-Tertiary sedimentary rocks overlain by Quaternary un-welded pyroclastic deposits, Old Alluvial deposits with debris flows units. Major slope movements within these areas are represented by the failure of unwelded pyroclastic flow deposits and unconsolidated old alluvial deposits accompanied with intense rainfall. Furthermore, these failures involve not only the rapid slide with fall of the pyroclastic flow deposits, but also include the rapid slide of the tephra and thick older alluvial deposits underlain by the deformed bedrocks. Most of these Large Scale Landslide features form by an aggregate of Smaller Landslide features and that movement could facilitate infiltration of groundwater into the head portion and the flank of landslide mass. Such conditions can cause localized instability and result in the formation of smaller landslides within the large landslide. Many of the currently existing active landslides represent reactivated portions of an old larger landslide masses in the Southern Kyushu regions. Further, it has been speculated that the landslide topography and material compositions of earth materials could also be modified when changes in the ground water flow regime. Finally, we discussed the relationship between landslide topography, mode of movement and mitigation measures according to the characteristics of each slope failures.
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Rocks of Singapore (2013)
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Geological Map of
Singapore (2009)
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Pyroclasts bearing Basaltic
Andesite PPL X.N X.N
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Planes: n=45 Strike: 87.7 Dip:
32.5 Pole trend: 357.7;Plung :57
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“The Best Geologist
is the one who has seen the most Rocks. “ (H. H. Read, 1940) Thank you!