"protolith" refers to the original composition of an altered rock. for example, a basalt was the protolith to a rock thats presently a greenschist.
The protolith of a metamorphic rock can be any pre-existing rock type, such as shale, limestone, basalt, or granite. The type of metamorphic rock that forms from a protolith depends on factors like temperature, pressure, and the mineral composition of the protolith.
Garnet gemstones are commonly found in various regions around the world including Africa, India, Brazil, and Australia. Additionally, garnets can also be found in the United States, with notable deposits in states such as Arizona and Idaho.
A protolith of sandstone is a sedimentary rock made up of sand-sized mineral grains or rock fragments that have been compacted and cemented together over time. It can form from the erosion and deposition of pre-existing rocks like granite, quartzite, or basalt.
The protolith of soapstone is usually ultramafic rocks such as serpentinite or peridotite. These rocks undergo metamorphism due to high heat and pressure, resulting in the formation of soapstone.
Garnet is a common component in well metamorphosed schists. Occasionally, a specimen will be good enough to be considered a jewel, but most garnet is valued as an abrasive - the garnet paper at your hardware store. There are about 20 various members of this family.
"protolith" refers to the original composition of an altered rock. for example, a basalt was the protolith to a rock thats presently a greenschist.
The protolith of a metamorphic rock can be any pre-existing rock type, such as shale, limestone, basalt, or granite. The type of metamorphic rock that forms from a protolith depends on factors like temperature, pressure, and the mineral composition of the protolith.
Mica schist is a metamorphic rock composed predominantly of mica minerals, typically biotite and muscovite, that exhibit a foliated texture. Phyllites are also metamorphic rocks with a fine-grained texture that is typically more dense and compact than schists. The protolith of both mica schist and phyllites is usually shale, mudstone, or other fine-grained sedimentary rocks that undergo metamorphism under heat and pressure.
Garnet gemstones are commonly found in various regions around the world including Africa, India, Brazil, and Australia. Additionally, garnets can also be found in the United States, with notable deposits in states such as Arizona and Idaho.
David Joseph Hall has written: 'Compositional variations in biotites and garnets from kyanite and sillimanite zone mica schists, Orange area, Massachusetts and New Hampshire' -- subject(s): Biotite, Garnet
peridotite
A protolith of sandstone is a sedimentary rock made up of sand-sized mineral grains or rock fragments that have been compacted and cemented together over time. It can form from the erosion and deposition of pre-existing rocks like granite, quartzite, or basalt.
The protolith of schist is typically shale or slate, which undergoes metamorphism to form schist. The protolith of anthracite coal is primarily bituminous coal, which is subjected to higher temperature and pressure conditions during metamorphism to convert into anthracite coal.
The protolith of marble was limestone or dolomite.
The protolith of marble was limestone or dolomite.
The protolith of phyllite is shale or mudstone that has been subjected to low-grade metamorphism. This metamorphic process causes the rock to recrystallize, resulting in a foliated texture with fine-grained mica minerals like muscovite and chlorite.