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Chapter 8: Major Elements - Faculty web pages

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Pressure-Temperature<br />

Temperature-Time Time (P-T-t) Paths<br />

<br />

The facies series concept suggests that a traverse up grade<br />

through a metamorphic terrane should follow a<br />

metamorphic field gradient, , and may cross through a<br />

sequence of facies<br />

<br />

Progressive metamorphism: rocks pass through a series of<br />

mineral assemblages as they continuously equilibrate to<br />

increasing metamorphic grade<br />

<br />

But does a rock in the upper amphibolite facies, for<br />

example, pass through the same sequence of mineral<br />

assemblages that are encountered via a traverse up grade<br />

to that rock through greenschist facies

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