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[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

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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