limestone and granite
Skarns are typically composed of minerals such as garnet, pyroxene, amphibole, epidote, and scapolite. They can also contain sulfide minerals like pyrite, chalcopyrite, and sphalerite, as well as carbonate minerals like calcite and dolomite. The exact chemical composition of a skarn can vary depending on the specific parent rock and the alteration processes that have occurred.
The parent rock (protolith) is the rock type that existed before a rock is altered into metamorphic rock. For instance, shale (sedimentary rock) is the parent rock of slate (metamorphic rock).
Limestone is the parent of rock of non foliated metamorphic. This is a very old type of rock.
It means the rock that a small piece broke off from. Outside our local library is a boulder quite different from our local sandstone. It is labelled as 'an erratic block of andesitic agglomerate' which broke off 'from the parent rock in Cumbria some millions of years ago'. It was carried about 120 miles by a glacier.
The parent rock of soapstone is typically serpentine. Soapstone forms when talc, a soft mineral, replaces the magnesium in the parent rock serpentine through a process called metasomatism.
Limestone doesn't normally have a parent rock. One exception to this may be a detrital limestone, whose parent rock would however also be limestone!
Skarn rock is primarily used in the mining and metallurgy industries, as it often contains valuable minerals such as copper, gold, and tungsten. The unique composition of skarn can also make it useful as a construction material, particularly in the production of concrete and aggregates. Additionally, skarn formations can serve as important geological indicators for the presence of mineral deposits, aiding exploration efforts.
Skarns are typically composed of minerals such as garnet, pyroxene, amphibole, epidote, and scapolite. They can also contain sulfide minerals like pyrite, chalcopyrite, and sphalerite, as well as carbonate minerals like calcite and dolomite. The exact chemical composition of a skarn can vary depending on the specific parent rock and the alteration processes that have occurred.
Skarn is metamorphic.
The metamorphosed limestone will most likely be a skarn or marble, both formed from contact with an intruding granitic magma.
Limestone does not have a parent rock.
Skarns are most often formed at the contact zone between intrusions of granitic magma bodies and carbonate sedimentary rocks such as limestone and dolostone.
Chert is a type of sedimentary rock made up of quartz and has a cryptocrystalline structure. It is often considered the parent rock of flint, jasper, and agate due to their similar composition and formation processes.
Limestone can metamorphose into marble, a regional metamorphic rock, or into skarn, a contact metamorphic rock.
David A John has written: 'Grade and tonnage model of tungsten skarn deposits, Nevada' -- subject(s): Ore deposits, Tungsten ores, Skarn
No, parent rock refers to the original rock from which soil is formed through weathering processes. Weathered rock particles are the result of the breakdown of parent rock due to physical, chemical, or biological processes.
Skarn forms from the alteration of carbonate rocks such as limestone or dolomite in the presence of hydrothermal fluids during contact metamorphism caused by intruding igneous rocks, typically granitic in composition. This process leads to the formation of a distinct mineral assemblage including garnet, pyroxene, and calc-silicate minerals.