SlideShare a Scribd company logo
1 of 8
[PRACTICAL PROSPECTOR'S GUIDE TO MINERALS]               October 3, 2012


        PRACTICAL PROSPECTOR'S GUIDE TO
                   MINERALS
                                 By

                     Prof. Dr. Hassan Z. Harraz
                        Geology Department
              Faculty Sciences, Tanta University-Egypt
                      hharraz2006@yahoo.com




Outline
        Topic 1:Rock-Forming Minerals
        Topic 2:Ores (Metallic)
        Topic 3:Ores (NON-Metallic)
        Topic 4:Industrial Minerals
        Topic 5:Gem Minerals




1Page                                                    HZH, Tanta Univ
[PRACTICAL PROSPECTOR'S GUIDE TO MINERALS]                            October 3, 2012




        PRACTICAL PROSPECTOR'S GUIDE TO
                   MINERALS

   I- Rock-Forming Minerals
    Quartz
             Most common mineral species
             Vitreous luster; conchoidal fracture; hexagonal, prismatic crystals are
              diagnostic
             Many color varieties: amethyst, smoky, rose, citrine
             Uses: glass manufacture, abrasive, flux, optical instruments,
              electronics

    Feldspar Group
      Potassium feldspars: microcline, orthoclase, sanidine
           blocky crystals, often show perthitic texture (especially microcline)
      Plagioclase feldspars: albite – anorthite series
           range from white to black
           often show play of colors (labradorescence)
           striations on cleavage surface (albite twinning)

    Mica Group
      Muscovite (white mica)
      Biotite (black mica)
      Phlogopite (brown mica)
      Sericite (brown to buff mica)
      Lepidolite (purple mica)
          lithium-rich pegmatites
          micaceous cleavage, elastic nature of plates and hardness distinguish
              micas from all other sheet-like minerals such as talc, gypsum and
              brucite

    Pyroxene Group
          Generally green to black (except spodumene, which can be white,
             yellowish, pink or green).
          2 good to perfect cleavages at nearly right angles (chief distinguishing
          characteristic between pyroxenes and amphiboles).
          Pyroxenes are common in mafic to ultramafic rocks and in skarns
          Emerald-green diopside (chrome-diopside) is a diamond indicator
             mineral
          Spodumene is a lithium pyroxene found in rare-element pegmatites
          Jadeite is one of the "true" jades and is a pyroxene

    Amphibole Group
     • Generally green to black (some, like tremolite, are white)


2Page                                                                HZH, Tanta Univ
[PRACTICAL PROSPECTOR'S GUIDE TO MINERALS]                              October 3, 2012


             2 good to perfect cleavages at 56 and 124 degrees (chief
              distinguishing
             characteristic between amphiboles and pyroxenes).
             BC jade is "nephrite", a variety actinolite, and is considered a "true"
              jade.
             amphiboles are common in skarns and in fairly high-grade
              metamorphic rocks.

    Garnet Group
      Almandine (iron – aluminum garnet)
          generally red
          found in schists
      Pyrope (magnesium – aluminum garnet)
          generally red
          diamond indicator mineral (kimberlites, lamprophyres)
      Spessartine (manganese – aluminum garnet)
          red to orange
          most often in rare-element pegmatites
      Grossular (calcium – aluminum garnet)
          brown, green, red, yellow
          often found in skarns
          gem brown variety known as "hessonite"
      Andradite (calcium – iron garnet)
          brown, green, red, yellow, black
          often found in skarns
          gem green variety could be "demantoid"
          titaniferous variety (black) is known as "melanite"
      Uvarovite (calcium – chromium garnet)
          chrome green
          associated with altered ultramafic rocks.

    Serpentine Group
          varied green color, greasy luster, often fibrous (or splintery)

    Olivine
             vitreous luster, conchoidal fracture, green color, presence in basalt as
              nodules

    Carbonate Group
      Calcite
                3 cleavages not at right angles
                fizzes readily with weak acid
      Siderite
                typical carbonate cleavage
                light to dark brown
      Dolomite
                curved, rhombohedral crystals
                     white, pink, gray

3Page                                                                 HZH, Tanta Univ
[PRACTICAL PROSPECTOR'S GUIDE TO MINERALS]                           October 3, 2012


II- Ores (Metallic)
A. Gold
B. Platinum Group Elements:
                   Platinum, Palladium, Iridium, Osmium
                   placer deposits, ultramafic rocks
C. Native Silver
                   wires in pockets, hackly fracture, tarnishes black
                   often as an impurity in galena
D. Sulfosalts
                   Pyrargyrite/Proustite (ruby silvers)
                   Stephanite
                   Tetrahedrite
E. Native Copper (100% Cu)
                   often in basalt; sometimes in oxidized zone; hackly fracture,
                    copper color
F. Chalcopyrite (35% Cu)
                   no cleavage, greenish-black streak, slightly greener yellow than
                    pyrite
G. Bornite (63% Cu)
                   purple-blue iridescent tarnish, BRONZY on FRESH
                    SURFACE
H. Covellite (66% Cu)
                   ELECTRIC BLUE, platy cleavage
I. Chalcocite (79% Cu)
                   black, SECTILE
J. Galena
                   3 perfect CLEAVAGES at right angles, DENSITY, lead-gray
                    color
                   secondary lead minerals: anglesite, cerussite, pyromorphite
J. Molybdenite
                   chief ore of molybdenum
                   SOFT, slightly bluer-gray than graphite (compare it with a
                    pencil ‘lead’)
L. Pyrite
                   often in good crystals (pyritohedra, cubes, octahedra); brittle,
                    black streak
M. Arsenopyrite
                   no cleavage, "garlic" smell sometimes when broken
N. Pyrrhotite
                   bronzy color, sometimes magnetic
O. Stibnite
                   main ore of antimony.
                   elongate crystals that are often ‘bent’; ONE PERFECT
                    CLEAVAGE and lower density distinguish it from galena.
                   will easily melt in a candle flame
P. Graphite
                     SOFT, black (like pencil "lead")

4Page                                                               HZH, Tanta Univ
[PRACTICAL PROSPECTOR'S GUIDE TO MINERALS]                                October 3, 2012


III- Ores (NON-Metallic)
A. Sphalerite
                     resinous to sub-metallic luster
                     yellow to green to red to black
                     Important ore of cadmium as well
                     alters to smithsonite, hydrozincite (fluorescent)
B. Wolframite
                     HEAVY, reddish to black, tabular crystals with one perfect
                      cleavage
C. Scheelite
                   White to brown, fluoresces bluish white
D. Manganese Oxides
                   psilomelane is a mixture of compact manganese oxides;
                      mixture of earthy manganese oxides is known as wad.
                   black, soft (often show dendritic stains)
E. Iron Oxides
                   mixture of iron oxides is generally known as limonite
      1. Hematite: red-brown streak
      2. Goethite: brown streak
F. Magnetite
                   black, dense, MAGNETIC
G. Cassiterite
                   black; glassy to resinous luster
H. Cinnabar
                   red; bright red streak; soft
I. Cuprite
                   red, often associated with malachite or other secondary copper
                      minerals
J. Malachite/Azurite
                   both are alteration products of other copper minerals
                   (MALACHITE is GREEN; AZURITE is BLUE (‘azure-blue’,
                      in fact)




5Page                                                                     HZH, Tanta Univ
[PRACTICAL PROSPECTOR'S GUIDE TO MINERALS]                              October 3, 2012


IV- Industrial Minerals
Diamond
                      as adamantine crystals in kimberlite or lamprophyre
                      placer deposits (weathered kimberlites/lamprophyres)
Sulfur
               as a native element in sedimentary rocks (often associated with
                petroleum)
Barite
                      one to two good cleavages, VERY heavy
                      in hydrothermal veins and sedimentary exhalative deposits
Gypsum
                      white to gray, softness is characteristic
                      sedimentary rocks
Magnesite
                      generally white
                      found most commonly in sedimentary rocks, but also in
                       carbonatites
                      hydromagnesite and epsomite are evaporites found in playa
                       lakes (from the alteration of volcanic rocks)

Apatite
                      hexagonal crystals, many colors
                      found in many environments
                      distinguished from beryl by its hardness (beryl cannot be
                       scratched by a knife)

Zeolite Group
                      generally white or off-white
                      found in volcanic rocks or low grade metamorphic rocks
                      economic deposits found as beds of altered volcanic ash
                      "boil" when torched

Fluorite
                      four directions of perfect CLEAVAGE

Corundum
                      HARDNESS of 9




6Page                                                                  HZH, Tanta Univ
[PRACTICAL PROSPECTOR'S GUIDE TO MINERALS]                               October 3, 2012


V- Gem Minerals
The following are reasonable to be expected, or have already been found in British
Columbia.

Corundum
              Ruby: red corundum coloured by chromium
              Sapphire: BLUE, green, pink, yellow, colourless corundum coloured
               by iron and/or titanium
Diamond

Beryl
              hexagonal cross-section; prismatic to tabular crystals; generally in
               pegmatites
Varieties of Beryl:
            Aquamarine: blue to green beryl coloured by iron
            Emerald: green beryl coloured by chromium or vanadium
            Goschenite: colourless beryl (originally cesium-bearing beryl)
            Heliodor: yellow beryl coloured by iron

Tourmaline
            diamond-shape cross-section; perfect basal cleavage (perpendicular to
               the length of the crystal)
Varieties of Gemmy Tourmaline:
            Schorl: black tourmaline found in simple pegmatites, hydrothermal
               veins and metamorphic rocks
            Elbaite: lithium-bearing tourmaline found almost exclusively in
               pegmatites;
            Rubellite (pink), Verdelite (green), Indicolite (blue), Achroite
               (colourless)
            Liddicoatite: another lithium-bearing tourmaline, again in pegmatites

Topaz
               diamond-shape cross-section; perfect basal cleavage (perpendicular to
                the length of the crystal)

Garnet
            metamorphic rocks; pegmatites
Varieties of Gemmy Garnet:
            Grossular: gem brown variety is hessonite
            Andradite: gem green variety is demantoid
            Spessartine: bright orange is best quality
Quartz
Varieties of Quartz:
            Amethyst: purple quartz coloured by iron (Fe4+)
            Citrine: yellow/orange quartz coloured by iron
            Smoky Quartz: brown to black quartz affected by radiation
            Rose Quartz: pink quartz coloured by manganese



7Page                                                                   HZH, Tanta Univ
[PRACTICAL PROSPECTOR'S GUIDE TO MINERALS]                          October 3, 2012


            Chalcedony: cryptocrystalline quartz; gray, greasy to silky luster;
             found in volcanic rocks and some sedimentary rocks
            Agate: concentrically banded chalcedony; variously coloured
            Onyx: flat, layered chalcedony; usually black/white or red/white<
            Carnelian: chalcedony coloured red by iron
            Chrysoprase: chalcedony coloured green by nickel
            Jasper: chalcedony coloured red, green, yellow or black by iron oxide

Opal
            in volcanic and sedimentary rocks
            common versus precious opal




8Page                                                              HZH, Tanta Univ

More Related Content

What's hot

skarn deposits and their mode of formation
skarn deposits and their mode of formationskarn deposits and their mode of formation
skarn deposits and their mode of formation
Adam Mbedzi
 

What's hot (20)

Classification of igneous rocks
Classification of igneous rocksClassification of igneous rocks
Classification of igneous rocks
 
Wall Rock Alteration.pdf
Wall Rock Alteration.pdfWall Rock Alteration.pdf
Wall Rock Alteration.pdf
 
Meteorites
MeteoritesMeteorites
Meteorites
 
Ch 10 magma generation
Ch 10 magma generationCh 10 magma generation
Ch 10 magma generation
 
SHEAR ZONE.pptx
SHEAR ZONE.pptxSHEAR ZONE.pptx
SHEAR ZONE.pptx
 
Anorthosite
Anorthosite Anorthosite
Anorthosite
 
Placer formation
Placer formationPlacer formation
Placer formation
 
Sedimentary Facies.ppt
Sedimentary Facies.pptSedimentary Facies.ppt
Sedimentary Facies.ppt
 
Ore deposit related to clastic sedimentation
Ore deposit related to clastic sedimentationOre deposit related to clastic sedimentation
Ore deposit related to clastic sedimentation
 
OLIVINE GROUP OF MINERALS
OLIVINE GROUP OF MINERALSOLIVINE GROUP OF MINERALS
OLIVINE GROUP OF MINERALS
 
Diversification of magma
Diversification of magmaDiversification of magma
Diversification of magma
 
volcanic exhalative process
volcanic exhalative processvolcanic exhalative process
volcanic exhalative process
 
Petrography study
Petrography studyPetrography study
Petrography study
 
FLUID INCLUSION WALL ROCK ALTERATION in economic geology
FLUID INCLUSION  WALL ROCK ALTERATION in economic geologyFLUID INCLUSION  WALL ROCK ALTERATION in economic geology
FLUID INCLUSION WALL ROCK ALTERATION in economic geology
 
Bowen reaction series and reaction principles
Bowen reaction series and reaction principles Bowen reaction series and reaction principles
Bowen reaction series and reaction principles
 
Igneous rocks
Igneous rocksIgneous rocks
Igneous rocks
 
Stuctural geology - Diapirs and Structural feautures By M.P. Billings
Stuctural geology -  Diapirs and Structural feautures By M.P. BillingsStuctural geology -  Diapirs and Structural feautures By M.P. Billings
Stuctural geology - Diapirs and Structural feautures By M.P. Billings
 
skarn deposits and their mode of formation
skarn deposits and their mode of formationskarn deposits and their mode of formation
skarn deposits and their mode of formation
 
Ch 11 diversification
Ch 11 diversificationCh 11 diversification
Ch 11 diversification
 
Kimberlites
KimberlitesKimberlites
Kimberlites
 

Similar to Practical prospector's guide to minerals

pegmatites minerals in Malawi
pegmatites minerals in Malawipegmatites minerals in Malawi
pegmatites minerals in Malawi
Grain Malunga
 
PHYSICAL GEOLOGY Minerals Chapter 3 1 Not count.docx
PHYSICAL GEOLOGY Minerals Chapter 3 1  Not count.docxPHYSICAL GEOLOGY Minerals Chapter 3 1  Not count.docx
PHYSICAL GEOLOGY Minerals Chapter 3 1 Not count.docx
mattjtoni51554
 
Gemstone Exploration & Mining
Gemstone Exploration & MiningGemstone Exploration & Mining
Gemstone Exploration & Mining
Sreevaru Surender
 

Similar to Practical prospector's guide to minerals (20)

Practical prospector's guide to minerals
Practical prospector's guide to mineralsPractical prospector's guide to minerals
Practical prospector's guide to minerals
 
Oxide Minerals
Oxide MineralsOxide Minerals
Oxide Minerals
 
pegmatites minerals in Malawi
pegmatites minerals in Malawipegmatites minerals in Malawi
pegmatites minerals in Malawi
 
Tourmaline, sapphire, peridot
Tourmaline, sapphire, peridotTourmaline, sapphire, peridot
Tourmaline, sapphire, peridot
 
Minerals ES
Minerals ESMinerals ES
Minerals ES
 
PHYSICAL GEOLOGY Minerals Chapter 3 1 Not count.docx
PHYSICAL GEOLOGY Minerals Chapter 3 1  Not count.docxPHYSICAL GEOLOGY Minerals Chapter 3 1  Not count.docx
PHYSICAL GEOLOGY Minerals Chapter 3 1 Not count.docx
 
Corundum
CorundumCorundum
Corundum
 
Gemstones
GemstonesGemstones
Gemstones
 
Gems
GemsGems
Gems
 
Epidote group
Epidote groupEpidote group
Epidote group
 
Spinel group and haematite group
Spinel group and haematite groupSpinel group and haematite group
Spinel group and haematite group
 
Gemstone Exploration & Mining
Gemstone Exploration & MiningGemstone Exploration & Mining
Gemstone Exploration & Mining
 
Phy properties of Minerals Part 1 VS.pptx
Phy properties of Minerals Part 1 VS.pptxPhy properties of Minerals Part 1 VS.pptx
Phy properties of Minerals Part 1 VS.pptx
 
MEMBERS OF AMPHIBOLE GROUP
MEMBERS OF AMPHIBOLE GROUPMEMBERS OF AMPHIBOLE GROUP
MEMBERS OF AMPHIBOLE GROUP
 
Garnet
GarnetGarnet
Garnet
 
Pyralspite
PyralspitePyralspite
Pyralspite
 
Shefa Yamem Poster 2006
Shefa Yamem Poster 2006Shefa Yamem Poster 2006
Shefa Yamem Poster 2006
 
Garnet, lapis class lecture
Garnet, lapis  class lectureGarnet, lapis  class lecture
Garnet, lapis class lecture
 
Common rock-forming minerals.pptx
Common rock-forming minerals.pptxCommon rock-forming minerals.pptx
Common rock-forming minerals.pptx
 
PRESENTATION ON GEOLOGY
PRESENTATION ON GEOLOGYPRESENTATION ON GEOLOGY
PRESENTATION ON GEOLOGY
 

More from Geology Department, Faculty of Science, Tanta University

Magnetization Roasting of Refractory Iron.pdf
Magnetization Roasting of Refractory Iron.pdfMagnetization Roasting of Refractory Iron.pdf
Magnetization Roasting of Refractory Iron.pdf
Geology Department, Faculty of Science, Tanta University
 
Direct Reduced Iron-Production.pdf
Direct Reduced Iron-Production.pdfDirect Reduced Iron-Production.pdf
A REVIEW OF IRONMAKING BY DIRECT REDUCTION PROCESSES.pdf
A REVIEW OF IRONMAKING BY DIRECT REDUCTION PROCESSES.pdfA REVIEW OF IRONMAKING BY DIRECT REDUCTION PROCESSES.pdf
A REVIEW OF IRONMAKING BY DIRECT REDUCTION PROCESSES.pdf
Geology Department, Faculty of Science, Tanta University
 
ENRICHMENT IRON BY REDUCTION ROASTING-MAGNETIC SEPARATION.pdf
ENRICHMENT IRON BY REDUCTION ROASTING-MAGNETIC SEPARATION.pdfENRICHMENT IRON BY REDUCTION ROASTING-MAGNETIC SEPARATION.pdf
ENRICHMENT IRON BY REDUCTION ROASTING-MAGNETIC SEPARATION.pdf
Geology Department, Faculty of Science, Tanta University
 
Processes for phosphorus removal from iron ore -.pdf
Processes for phosphorus removal from iron ore -.pdfProcesses for phosphorus removal from iron ore -.pdf
Processes for phosphorus removal from iron ore -.pdf
Geology Department, Faculty of Science, Tanta University
 

More from Geology Department, Faculty of Science, Tanta University (20)

ESSENTIALS OF IRON ORE DEPOSITS and INDUSTRIES.pdf
ESSENTIALS OF IRON ORE DEPOSITS and INDUSTRIES.pdfESSENTIALS OF IRON ORE DEPOSITS and INDUSTRIES.pdf
ESSENTIALS OF IRON ORE DEPOSITS and INDUSTRIES.pdf
 
Minerals phase transformation by hydrogen reduction.pdf
Minerals phase transformation by hydrogen reduction.pdfMinerals phase transformation by hydrogen reduction.pdf
Minerals phase transformation by hydrogen reduction.pdf
 
Magnetization Roasting of Refractory Iron.pdf
Magnetization Roasting of Refractory Iron.pdfMagnetization Roasting of Refractory Iron.pdf
Magnetization Roasting of Refractory Iron.pdf
 
GLOBAL IRON ORE.pdf
GLOBAL IRON ORE.pdfGLOBAL IRON ORE.pdf
GLOBAL IRON ORE.pdf
 
Ferrous Scrap FUTURE.pdf
Ferrous Scrap  FUTURE.pdfFerrous Scrap  FUTURE.pdf
Ferrous Scrap FUTURE.pdf
 
Pelletizing Process.pdf
Pelletizing Process.pdfPelletizing Process.pdf
Pelletizing Process.pdf
 
Direct Reduced Iron-Production.pdf
Direct Reduced Iron-Production.pdfDirect Reduced Iron-Production.pdf
Direct Reduced Iron-Production.pdf
 
A REVIEW OF IRONMAKING BY DIRECT REDUCTION PROCESSES.pdf
A REVIEW OF IRONMAKING BY DIRECT REDUCTION PROCESSES.pdfA REVIEW OF IRONMAKING BY DIRECT REDUCTION PROCESSES.pdf
A REVIEW OF IRONMAKING BY DIRECT REDUCTION PROCESSES.pdf
 
IRONWORKS.pdf
IRONWORKS.pdfIRONWORKS.pdf
IRONWORKS.pdf
 
ENRICHMENT IRON BY REDUCTION ROASTING-MAGNETIC SEPARATION.pdf
ENRICHMENT IRON BY REDUCTION ROASTING-MAGNETIC SEPARATION.pdfENRICHMENT IRON BY REDUCTION ROASTING-MAGNETIC SEPARATION.pdf
ENRICHMENT IRON BY REDUCTION ROASTING-MAGNETIC SEPARATION.pdf
 
Processes for phosphorus removal from iron ore -.pdf
Processes for phosphorus removal from iron ore -.pdfProcesses for phosphorus removal from iron ore -.pdf
Processes for phosphorus removal from iron ore -.pdf
 
Iron Types-HBI-DRI.pdf
Iron Types-HBI-DRI.pdfIron Types-HBI-DRI.pdf
Iron Types-HBI-DRI.pdf
 
IRON ORE DEPOSITS.pdf
IRON ORE DEPOSITS.pdfIRON ORE DEPOSITS.pdf
IRON ORE DEPOSITS.pdf
 
STEEL INDUSTRY IN EGYPT-Companies and Markets.pdf
STEEL INDUSTRY IN EGYPT-Companies and Markets.pdfSTEEL INDUSTRY IN EGYPT-Companies and Markets.pdf
STEEL INDUSTRY IN EGYPT-Companies and Markets.pdf
 
Cv english-harraz
Cv english-harrazCv english-harraz
Cv english-harraz
 
Rodruin prospecting area conf
Rodruin prospecting area confRodruin prospecting area conf
Rodruin prospecting area conf
 
Crusher; Crushing; and Classification Equipment
Crusher; Crushing; and Classification EquipmentCrusher; Crushing; and Classification Equipment
Crusher; Crushing; and Classification Equipment
 
The garnet group
The garnet groupThe garnet group
The garnet group
 
Hydrothermal alterations
Hydrothermal alterationsHydrothermal alterations
Hydrothermal alterations
 
Lecture 10 textures of ore deposits and associated features
Lecture 10 textures of ore deposits and associated featuresLecture 10 textures of ore deposits and associated features
Lecture 10 textures of ore deposits and associated features
 

Recently uploaded

Biogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune Waterworlds
Biogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune WaterworldsBiogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune Waterworlds
Biogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune Waterworlds
Sérgio Sacani
 
CYTOGENETIC MAP................ ppt.pptx
CYTOGENETIC MAP................ ppt.pptxCYTOGENETIC MAP................ ppt.pptx
CYTOGENETIC MAP................ ppt.pptx
Silpa
 
biology HL practice questions IB BIOLOGY
biology HL practice questions IB BIOLOGYbiology HL practice questions IB BIOLOGY
biology HL practice questions IB BIOLOGY
1301aanya
 
THE ROLE OF BIOTECHNOLOGY IN THE ECONOMIC UPLIFT.pptx
THE ROLE OF BIOTECHNOLOGY IN THE ECONOMIC UPLIFT.pptxTHE ROLE OF BIOTECHNOLOGY IN THE ECONOMIC UPLIFT.pptx
THE ROLE OF BIOTECHNOLOGY IN THE ECONOMIC UPLIFT.pptx
ANSARKHAN96
 

Recently uploaded (20)

PATNA CALL GIRLS 8617370543 LOW PRICE ESCORT SERVICE
PATNA CALL GIRLS 8617370543 LOW PRICE ESCORT SERVICEPATNA CALL GIRLS 8617370543 LOW PRICE ESCORT SERVICE
PATNA CALL GIRLS 8617370543 LOW PRICE ESCORT SERVICE
 
TransientOffsetin14CAftertheCarringtonEventRecordedbyPolarTreeRings
TransientOffsetin14CAftertheCarringtonEventRecordedbyPolarTreeRingsTransientOffsetin14CAftertheCarringtonEventRecordedbyPolarTreeRings
TransientOffsetin14CAftertheCarringtonEventRecordedbyPolarTreeRings
 
CURRENT SCENARIO OF POULTRY PRODUCTION IN INDIA
CURRENT SCENARIO OF POULTRY PRODUCTION IN INDIACURRENT SCENARIO OF POULTRY PRODUCTION IN INDIA
CURRENT SCENARIO OF POULTRY PRODUCTION IN INDIA
 
Biogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune Waterworlds
Biogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune WaterworldsBiogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune Waterworlds
Biogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune Waterworlds
 
Thyroid Physiology_Dr.E. Muralinath_ Associate Professor
Thyroid Physiology_Dr.E. Muralinath_ Associate ProfessorThyroid Physiology_Dr.E. Muralinath_ Associate Professor
Thyroid Physiology_Dr.E. Muralinath_ Associate Professor
 
Site Acceptance Test .
Site Acceptance Test                    .Site Acceptance Test                    .
Site Acceptance Test .
 
Chemistry 5th semester paper 1st Notes.pdf
Chemistry 5th semester paper 1st Notes.pdfChemistry 5th semester paper 1st Notes.pdf
Chemistry 5th semester paper 1st Notes.pdf
 
module for grade 9 for distance learning
module for grade 9 for distance learningmodule for grade 9 for distance learning
module for grade 9 for distance learning
 
CYTOGENETIC MAP................ ppt.pptx
CYTOGENETIC MAP................ ppt.pptxCYTOGENETIC MAP................ ppt.pptx
CYTOGENETIC MAP................ ppt.pptx
 
biology HL practice questions IB BIOLOGY
biology HL practice questions IB BIOLOGYbiology HL practice questions IB BIOLOGY
biology HL practice questions IB BIOLOGY
 
FAIRSpectra - Enabling the FAIRification of Spectroscopy and Spectrometry
FAIRSpectra - Enabling the FAIRification of Spectroscopy and SpectrometryFAIRSpectra - Enabling the FAIRification of Spectroscopy and Spectrometry
FAIRSpectra - Enabling the FAIRification of Spectroscopy and Spectrometry
 
FAIRSpectra - Enabling the FAIRification of Analytical Science
FAIRSpectra - Enabling the FAIRification of Analytical ScienceFAIRSpectra - Enabling the FAIRification of Analytical Science
FAIRSpectra - Enabling the FAIRification of Analytical Science
 
Factory Acceptance Test( FAT).pptx .
Factory Acceptance Test( FAT).pptx       .Factory Acceptance Test( FAT).pptx       .
Factory Acceptance Test( FAT).pptx .
 
Atp synthase , Atp synthase complex 1 to 4.
Atp synthase , Atp synthase complex 1 to 4.Atp synthase , Atp synthase complex 1 to 4.
Atp synthase , Atp synthase complex 1 to 4.
 
Climate Change Impacts on Terrestrial and Aquatic Ecosystems.pptx
Climate Change Impacts on Terrestrial and Aquatic Ecosystems.pptxClimate Change Impacts on Terrestrial and Aquatic Ecosystems.pptx
Climate Change Impacts on Terrestrial and Aquatic Ecosystems.pptx
 
THE ROLE OF BIOTECHNOLOGY IN THE ECONOMIC UPLIFT.pptx
THE ROLE OF BIOTECHNOLOGY IN THE ECONOMIC UPLIFT.pptxTHE ROLE OF BIOTECHNOLOGY IN THE ECONOMIC UPLIFT.pptx
THE ROLE OF BIOTECHNOLOGY IN THE ECONOMIC UPLIFT.pptx
 
PSYCHOSOCIAL NEEDS. in nursing II sem pptx
PSYCHOSOCIAL NEEDS. in nursing II sem pptxPSYCHOSOCIAL NEEDS. in nursing II sem pptx
PSYCHOSOCIAL NEEDS. in nursing II sem pptx
 
Genome sequencing,shotgun sequencing.pptx
Genome sequencing,shotgun sequencing.pptxGenome sequencing,shotgun sequencing.pptx
Genome sequencing,shotgun sequencing.pptx
 
Dr. E. Muralinath_ Blood indices_clinical aspects
Dr. E. Muralinath_ Blood indices_clinical  aspectsDr. E. Muralinath_ Blood indices_clinical  aspects
Dr. E. Muralinath_ Blood indices_clinical aspects
 
Zoology 5th semester notes( Sumit_yadav).pdf
Zoology 5th semester notes( Sumit_yadav).pdfZoology 5th semester notes( Sumit_yadav).pdf
Zoology 5th semester notes( Sumit_yadav).pdf
 

Practical prospector's guide to minerals

  • 1. [PRACTICAL PROSPECTOR'S GUIDE TO MINERALS] October 3, 2012 PRACTICAL PROSPECTOR'S GUIDE TO MINERALS By Prof. Dr. Hassan Z. Harraz Geology Department Faculty Sciences, Tanta University-Egypt hharraz2006@yahoo.com Outline Topic 1:Rock-Forming Minerals Topic 2:Ores (Metallic) Topic 3:Ores (NON-Metallic) Topic 4:Industrial Minerals Topic 5:Gem Minerals 1Page HZH, Tanta Univ
  • 2. [PRACTICAL PROSPECTOR'S GUIDE TO MINERALS] October 3, 2012 PRACTICAL PROSPECTOR'S GUIDE TO MINERALS I- Rock-Forming Minerals Quartz  Most common mineral species  Vitreous luster; conchoidal fracture; hexagonal, prismatic crystals are diagnostic  Many color varieties: amethyst, smoky, rose, citrine  Uses: glass manufacture, abrasive, flux, optical instruments, electronics Feldspar Group Potassium feldspars: microcline, orthoclase, sanidine  blocky crystals, often show perthitic texture (especially microcline) Plagioclase feldspars: albite – anorthite series  range from white to black  often show play of colors (labradorescence)  striations on cleavage surface (albite twinning) Mica Group Muscovite (white mica) Biotite (black mica) Phlogopite (brown mica) Sericite (brown to buff mica) Lepidolite (purple mica)  lithium-rich pegmatites  micaceous cleavage, elastic nature of plates and hardness distinguish micas from all other sheet-like minerals such as talc, gypsum and brucite Pyroxene Group  Generally green to black (except spodumene, which can be white, yellowish, pink or green).  2 good to perfect cleavages at nearly right angles (chief distinguishing  characteristic between pyroxenes and amphiboles).  Pyroxenes are common in mafic to ultramafic rocks and in skarns  Emerald-green diopside (chrome-diopside) is a diamond indicator mineral  Spodumene is a lithium pyroxene found in rare-element pegmatites  Jadeite is one of the "true" jades and is a pyroxene Amphibole Group • Generally green to black (some, like tremolite, are white) 2Page HZH, Tanta Univ
  • 3. [PRACTICAL PROSPECTOR'S GUIDE TO MINERALS] October 3, 2012  2 good to perfect cleavages at 56 and 124 degrees (chief distinguishing  characteristic between amphiboles and pyroxenes).  BC jade is "nephrite", a variety actinolite, and is considered a "true" jade.  amphiboles are common in skarns and in fairly high-grade metamorphic rocks. Garnet Group Almandine (iron – aluminum garnet)  generally red  found in schists Pyrope (magnesium – aluminum garnet)  generally red  diamond indicator mineral (kimberlites, lamprophyres) Spessartine (manganese – aluminum garnet)  red to orange  most often in rare-element pegmatites Grossular (calcium – aluminum garnet)  brown, green, red, yellow  often found in skarns  gem brown variety known as "hessonite" Andradite (calcium – iron garnet)  brown, green, red, yellow, black  often found in skarns  gem green variety could be "demantoid"  titaniferous variety (black) is known as "melanite" Uvarovite (calcium – chromium garnet)  chrome green  associated with altered ultramafic rocks. Serpentine Group  varied green color, greasy luster, often fibrous (or splintery) Olivine  vitreous luster, conchoidal fracture, green color, presence in basalt as nodules Carbonate Group Calcite  3 cleavages not at right angles  fizzes readily with weak acid Siderite  typical carbonate cleavage  light to dark brown Dolomite  curved, rhombohedral crystals  white, pink, gray 3Page HZH, Tanta Univ
  • 4. [PRACTICAL PROSPECTOR'S GUIDE TO MINERALS] October 3, 2012 II- Ores (Metallic) A. Gold B. Platinum Group Elements:  Platinum, Palladium, Iridium, Osmium  placer deposits, ultramafic rocks C. Native Silver  wires in pockets, hackly fracture, tarnishes black  often as an impurity in galena D. Sulfosalts  Pyrargyrite/Proustite (ruby silvers)  Stephanite  Tetrahedrite E. Native Copper (100% Cu)  often in basalt; sometimes in oxidized zone; hackly fracture, copper color F. Chalcopyrite (35% Cu)  no cleavage, greenish-black streak, slightly greener yellow than pyrite G. Bornite (63% Cu)  purple-blue iridescent tarnish, BRONZY on FRESH SURFACE H. Covellite (66% Cu)  ELECTRIC BLUE, platy cleavage I. Chalcocite (79% Cu)  black, SECTILE J. Galena  3 perfect CLEAVAGES at right angles, DENSITY, lead-gray color  secondary lead minerals: anglesite, cerussite, pyromorphite J. Molybdenite  chief ore of molybdenum  SOFT, slightly bluer-gray than graphite (compare it with a pencil ‘lead’) L. Pyrite  often in good crystals (pyritohedra, cubes, octahedra); brittle, black streak M. Arsenopyrite  no cleavage, "garlic" smell sometimes when broken N. Pyrrhotite  bronzy color, sometimes magnetic O. Stibnite  main ore of antimony.  elongate crystals that are often ‘bent’; ONE PERFECT CLEAVAGE and lower density distinguish it from galena.  will easily melt in a candle flame P. Graphite  SOFT, black (like pencil "lead") 4Page HZH, Tanta Univ
  • 5. [PRACTICAL PROSPECTOR'S GUIDE TO MINERALS] October 3, 2012 III- Ores (NON-Metallic) A. Sphalerite  resinous to sub-metallic luster  yellow to green to red to black  Important ore of cadmium as well  alters to smithsonite, hydrozincite (fluorescent) B. Wolframite  HEAVY, reddish to black, tabular crystals with one perfect cleavage C. Scheelite  White to brown, fluoresces bluish white D. Manganese Oxides  psilomelane is a mixture of compact manganese oxides; mixture of earthy manganese oxides is known as wad.  black, soft (often show dendritic stains) E. Iron Oxides  mixture of iron oxides is generally known as limonite 1. Hematite: red-brown streak 2. Goethite: brown streak F. Magnetite  black, dense, MAGNETIC G. Cassiterite  black; glassy to resinous luster H. Cinnabar  red; bright red streak; soft I. Cuprite  red, often associated with malachite or other secondary copper minerals J. Malachite/Azurite  both are alteration products of other copper minerals  (MALACHITE is GREEN; AZURITE is BLUE (‘azure-blue’, in fact) 5Page HZH, Tanta Univ
  • 6. [PRACTICAL PROSPECTOR'S GUIDE TO MINERALS] October 3, 2012 IV- Industrial Minerals Diamond  as adamantine crystals in kimberlite or lamprophyre  placer deposits (weathered kimberlites/lamprophyres) Sulfur  as a native element in sedimentary rocks (often associated with petroleum) Barite  one to two good cleavages, VERY heavy  in hydrothermal veins and sedimentary exhalative deposits Gypsum  white to gray, softness is characteristic  sedimentary rocks Magnesite  generally white  found most commonly in sedimentary rocks, but also in carbonatites  hydromagnesite and epsomite are evaporites found in playa lakes (from the alteration of volcanic rocks) Apatite  hexagonal crystals, many colors  found in many environments  distinguished from beryl by its hardness (beryl cannot be scratched by a knife) Zeolite Group  generally white or off-white  found in volcanic rocks or low grade metamorphic rocks  economic deposits found as beds of altered volcanic ash  "boil" when torched Fluorite  four directions of perfect CLEAVAGE Corundum  HARDNESS of 9 6Page HZH, Tanta Univ
  • 7. [PRACTICAL PROSPECTOR'S GUIDE TO MINERALS] October 3, 2012 V- Gem Minerals The following are reasonable to be expected, or have already been found in British Columbia. Corundum  Ruby: red corundum coloured by chromium  Sapphire: BLUE, green, pink, yellow, colourless corundum coloured by iron and/or titanium Diamond Beryl  hexagonal cross-section; prismatic to tabular crystals; generally in pegmatites Varieties of Beryl:  Aquamarine: blue to green beryl coloured by iron  Emerald: green beryl coloured by chromium or vanadium  Goschenite: colourless beryl (originally cesium-bearing beryl)  Heliodor: yellow beryl coloured by iron Tourmaline  diamond-shape cross-section; perfect basal cleavage (perpendicular to the length of the crystal) Varieties of Gemmy Tourmaline:  Schorl: black tourmaline found in simple pegmatites, hydrothermal veins and metamorphic rocks  Elbaite: lithium-bearing tourmaline found almost exclusively in pegmatites;  Rubellite (pink), Verdelite (green), Indicolite (blue), Achroite (colourless)  Liddicoatite: another lithium-bearing tourmaline, again in pegmatites Topaz  diamond-shape cross-section; perfect basal cleavage (perpendicular to the length of the crystal) Garnet  metamorphic rocks; pegmatites Varieties of Gemmy Garnet:  Grossular: gem brown variety is hessonite  Andradite: gem green variety is demantoid  Spessartine: bright orange is best quality Quartz Varieties of Quartz:  Amethyst: purple quartz coloured by iron (Fe4+)  Citrine: yellow/orange quartz coloured by iron  Smoky Quartz: brown to black quartz affected by radiation  Rose Quartz: pink quartz coloured by manganese 7Page HZH, Tanta Univ
  • 8. [PRACTICAL PROSPECTOR'S GUIDE TO MINERALS] October 3, 2012  Chalcedony: cryptocrystalline quartz; gray, greasy to silky luster; found in volcanic rocks and some sedimentary rocks  Agate: concentrically banded chalcedony; variously coloured  Onyx: flat, layered chalcedony; usually black/white or red/white<  Carnelian: chalcedony coloured red by iron  Chrysoprase: chalcedony coloured green by nickel  Jasper: chalcedony coloured red, green, yellow or black by iron oxide Opal  in volcanic and sedimentary rocks  common versus precious opal 8Page HZH, Tanta Univ