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Garnet generally forms at greater depths compared to chlorite. Garnet is commonly found in high-grade metamorphic rocks and is stable at higher pressures and temperatures, typically occurring in depths of 20 to 40 kilometers in the Earth's crust. In contrast, chlorite forms in lower-grade metamorphic environments and is typically found at shallower depths, usually within the upper crust. Thus, garnet has a greater depth of formation than chlorite.

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What rock forms deeper garnet or chlorite?

Garnet is indicative of deeper metamorphism than chlorite.


What is farther down than chlorite and heated to temperatures less than garnet?

In the context of metamorphic grade, biotite is typically found farther down than chlorite and is stable at temperatures lower than those required for garnet formation. Biotite forms in the medium-grade metamorphic conditions, while garnet forms in higher-grade conditions. Thus, biotite represents a transitional mineral between chlorite and garnet in metamorphic rocks.


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If you had two metamorphic rocksone with garnet crystals and the other with chlorite crystals which one would have formed at a deeper level in earth's crust?

The metamorphic rock with garnet crystals would have formed at a deeper level in the Earth's crust compared to the one with chlorite crystals. Garnet is a high-pressure mineral that forms under conditions of high temperature and pressure, typically found deeper in the crust. Chlorite, on the other hand, is indicative of lower-grade metamorphism and forms at shallower depths. Therefore, the presence of garnet suggests a rock that has undergone more intense metamorphism at greater depths.


Farther down than chlorite heated to temperatures less than garnet?

In metamorphic processes, chlorite typically forms at lower temperatures and pressures than garnet. When chlorite is subjected to heating at temperatures lower than those required for garnet formation, it can dehydrate and transform into other minerals such as biotite or muscovite, depending on the specific conditions. This transition occurs in the context of regional metamorphism, where temperature and pressure conditions dictate the stability of various mineral assemblages. Therefore, farther down in the metamorphic gradient, chlorite will not persist but will instead yield to higher-grade minerals.


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