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  2. Sanidine - Wikipedia

    en.wikipedia.org/wiki/Sanidine

    Sanidine is the high temperature form of potassium feldspar with a general formula K(AlSi 3 O 8). [2] Sanidine is found most typically in felsic volcanic rocks such as obsidian, rhyolite and trachyte. Sanidine crystallizes in the monoclinic crystal system. Orthoclase is a monoclinic polymorph stable at lower temperatures.

  3. Orthoclase - Wikipedia

    en.wikipedia.org/wiki/Orthoclase

    Orthoclase, or orthoclase feldspar (endmember formula K Al Si 3 O 8), is an important tectosilicate mineral which forms igneous rock. The name is from the Ancient Greek for "straight fracture", because its two cleavage planes are at right angles to each other. It is a type of potassium feldspar, also known as K-feldspar.

  4. Feldspar - Wikipedia

    en.wikipedia.org/wiki/Feldspar

    Feldspar (/ ˈ f ɛ l (d) ˌ s p ɑːr / FEL(D)-spar; sometimes spelled felspar) is a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium. [3] The most common members of the feldspar group are the plagioclase (sodium-calcium) feldspars and the alkali (potassium ...

  5. Perthite - Wikipedia

    en.wikipedia.org/wiki/Perthite

    If cooling is sufficiently slow, the alkali feldspar may exsolve to form separate grains with near-endmember albite and K-feldspar compositions. The largest documented single crystal of perthite was found in Hugo Mine in South Dakota and measured about 10.7 m (35 ft) × 4.6 m (15 ft) × 1.8 m (5 ft 11 in).

  6. Folk classification - Wikipedia

    en.wikipedia.org/wiki/Folk_classification

    If the abundances of quartz, feldspars and rock fragments indicate that the rock is an arkose, a subarkose or a lithic arkose, one must then normalize the abundance of feldspars to 100% and attempt to identify the relative abundances of K-feldspars to plagioclase in the sample. If there is more plagioclase than there is K-feldspar, the rock is ...

  7. Metamorphic facies - Wikipedia

    en.wikipedia.org/wiki/Metamorphic_facies

    cordierite + quartz + sillimanite + K-feldspar (orthoclase) ± biotite ± garnet (If the temperature is below 750 °C there will be andalusite instead of sillimanite) cordierite + orthopyroxene + plagioclase ± garnet, spinel; In carbonate rocks: calcite + forsterite ± diopside, periclase; diopside + grossular + wollastonite ± vesuvianite