The Mineral Facies of Rocks¶
Eskola, P. (1920). The Mineral Facies of Rocks.
Cited by¶
1 citation across 1 artifact.
Domain-specific¶
- Metamorphism
- Metamorphic facies (zeolite, greenschist, amphibolite, granulite, eclogite, blueschist) are regions of pressure-temperature space within which a specific range of mineral assemblages is stable, and assigning a rock to a facies constrains the conditions under which it formed
Supported in partVerified against the source
- Metamorphic facies (zeolite, greenschist, amphibolite, granulite, eclogite, blueschist) are regions of pressure-temperature space within which a specific range of mineral assemblages is stable, and assigning a rock to a facies constrains the conditions under which it formed
Verification¶
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Registry ID ref:1ac804c04b4e · see in the full table