問題一覧
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Ca-rich amphibole mineral, common in diorites, commonly occurs with pagioclase
Hornblende
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•Potassium Feldspar/ Orthoclase/ Alkali Feldspar • Calcium Feldspar/ Pagioclase • Sodium Feldspar / Albite
Feldspars
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common in granite, diorite and chert
Quartz
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Monoclinic Augite
Clinopyroxene
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Most abundunt silicate mineral in the crust
Calcium Feldspar/ Pagioclase
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Contain (CO3)2-
Carbonates
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3D framework if silicate tetrahedron Feldspar Silica Group
Tectosilicates
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Dark colored mica common in granite, diorite, gabbros, and peridotites
Biotite
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Strong Ionic bonding,hard, dense, and refractory
Oxides
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Commonly deposited in marine settings when the shells of dead planktonic life settle and accumulate on the sea floor
Carbonates
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Rose,admethyst and smoky ____ are low temp varieties
Quartz
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In metamorphic rocks, it occurs with chlorite and muscovite
Biotite
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common in gangue mineral in hydrothermal ore deposit
Quartz
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Mg-rich if in unltramafics and Fe-rich if in granites
Biotite
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Quartz, Opal , Chalcedony
Silica Group
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______ minerals make up over 90% of crust
Silicates
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• Hornblende • cleavage: 2 at 60 deg and 120 deg • in the presence of water/fluids, pyroxenes are often converted to amphibole
Double/ Amphibole group
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Form at low temp, and predominantly in weathering products (alteration in hydrothermal veins)
Hydroxides
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Contains halogen ions like Cl- or F-
Halides
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Similar structure with silicates but instead of Si, its P, As (arsenates), or Va (Vanadates)
Phosphates
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Can be simple or multiple
Oxides
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Single, isolated tetrahedron No cleavage Composition: (Mg, Fe)2SiO4
Neosilicates/ Olivine Group
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turquoise
Phosphates
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not stable in the presence of free quartz and will form a pyroxene called enstatite
Forsterite
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Most common pyroxene mineral
Augite
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Sheets of silicate tetrahedron cleavage: 1 plane Biotite Muscovite
Phyilosilicates/ Mica Group
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Metal cations combined with oxygen
Oxides
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Economically important as metal ores
Sulfides
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Halite(NaCl), Flourite (CaF2), Sylvite KCl
Halides
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S2- bonded to metal cation
Sulfides
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Cu,Au,Ag,S,Diamond
Native Elements
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Salts that form when salt water evaporates
Halides
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•Structure possessing parallel silica letrahedron chains whuch can be double or single • Single/Pyroxene Group • Double/ Amphibole Group
Inosilicates
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Gypsum, Barite
Sulfates
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along with chalcedony and agate, they occur in hydrothermally altered rocks
Opal
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Quartz with water
Opal
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Cleavage: 2 at 90 deg Orthopyroxene Clinopyroxene
Single/ pyroxene Group
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Silica Tetrahedon, as fundamental component
Silicates
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Common in peridotites, gabbros, norutes and basalts Commonly associated by olivine, pagioclase, Ca-rich clinopyroxene
Enstatite
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Low hardness, poor thermal and electric conductors when solid, good electric conductors when molten
Halides
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pyrite, galena
Sulfides
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Also carry the best record of changes in the earths magnetic field
Oxides
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Metals attached with (OH)-
Hydroxides
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Tend to be less dense than oxides, and not as hard
Hydroxides
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(SO4)2- bonded to metal action
Sulfates
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Pure masses if single metal/ element
Native Elements
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Hematite, Magnetite, Chromite, Pyrolusite, manganite
Oxides
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Occur in native state, uncombined form
Native Elements
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Manganite (MnO(OH)), diaspore, Geothite
Hydroxides
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Tridymite or cristobalite in high temp
Quartz
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Calcite, Azurite, Malachite, dolomite
Carbonates
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Form many of the valuable ores
Oxides
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Light colored mica common in granites
Muscovite
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Many forms by precipitation out of highly saline water at and/or near the Earths surface
Sulfates
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Fibrous Variety
Chalcedony