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greenschist facies

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greenschist facies

One of the major divisions of the mineral facies classification of metamorphic rocks, encompassing the rocks that formed under fairly low temperatures (480–660 °F, or 250–350 °C) and pressure conditions and usually produced by regional metamorphism. The minerals commonly found in such rocks include quartz, orthoclase, muscovite, chlorite, serpentine, talc, and epidote; carbonate minerals and amphibole (actinolite) may also be present.


greenschist facies [′grēn‚shist ′fā·shēz]
(petrology)
Any schistose rock containing an abundance of green minerals and produced under conditions of low to intermediate temperatures (300-500°C) and low to moderate hydrostatic pressures (3000-8000 bars).


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The third group (sedimentary and carbonate rocks) is suggested to consist of epithermal gold deposits in lower greenschist facies rocks and distal to any known igneous rocks.
The hydrothermal alteration of the samples varies from literally fresh rocks to true greenschist facies rocks.
It contains terrigenous sedimentary rocks, mafic to ultramafic volcanic rocks and plutonic rocks metamorphosed from the greenschist facies to the lower amphibolite facies.
 
 
 
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