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28 Cards in this Set

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  • Back
K-feldspar
K-feldspar
Potassium feldspars are a group of polymorphs, polymorphs being minerals that have the same chemical composition but slightly different crystal structures
K-feldspar
K-feldspar
When combined with water during hydrolysis it creates clay minerals (hydrous Al silicates)
Plagioclase feldspar
Plagioclase feldspar
Plagioclase feldspars are a continuous mineral series in which calcium and sodium substitute for one another in the same crystal structure, dissociates with water in order to create acids in soils
Quartz
Quartz
one of the most common minerals because it is chemically and physically stable at Earth’s surface conditions. It is a significant component of hydrothermal veins and felsic igneous rocks, and is often the dominant mineral in sandstones and siltstones,
Quartz
Quartz
More resistant to weathering than the feldspar groups, also immobile.
Kaolinite
Kaolinite
Al2Si2O5(OH)4
Pyrite
Pyrite
FeS2
Pyrite
Pyrite
Pyrite ---> Hematite
2Fe(+2)S2(-4) + O2 ---> Fe2(+3)O3(+2) + 2S(-4)
Hematite
Hematite
Fe2O3
Hematite
Hematite
Branded Iron formations are proof of the difference between the reducing and oxidizing environments prior before and after The Great Oxidation Events
Magnetite
Calcite
Calcite
Often found in limestone
Aragonite
Aragonite
crystal lattice differs from that of calcite, resulting in a different crystal shape, an orthorhombic system with acicular crystals
Dolomite
Dolomite
The best way to tell one from the other is the acid test: a drop of 1 M HCl on calcite produces an instant, obvious fizz; a drop on dolomite produces slow or no obvious bubbling
Dolomite
CaMg(CO3)2, Magnesium makes it more resistant to HCl
Zircon
Zircon
One of the most resistant minerals zircons can survive geologic processes like erosion, transport, even high-grade metamorphism, they contain a rich and varied record of geological processes. Radiometric dating of Uranium to Lead.
Plagioclase feldspar
Plagioclase feldspar
will weather to form clay minerals, they are resistant enough that plagioclase grains forms a significant component of many detrital sediments and sedimentary rocks.
Halite
Barite
Orthoclase
Goethite
Limonite
Garnet
Garnet
Garnet
Spharelite
Galena
Chlorite
Bauxite
Biotite