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Chapter 26: Metamorphic Reactions

Chapter 26: Metamorphic Reactions. If we treat isograds as reactions, we can: Understand what physical variables might affect the location of a particular isograd We may also be able to estimate the P-T-X conditions that an isograd represents.

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Calcareous and Ultramafic Rocks

Calcareous and Ultramafic Rocks. Reading: Winter Chapter 29. Calcareous Metamorphic Rocks. Calcareous rocks are predominantly carbonates, usually limestone or dolostone Typically form in a stable continental shelf environment along a passive margin

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Chapter 26: Metamorphic Reactions

Calcareous and Ultramafic Rocks