A proposed subdivision of the granulite facies
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ID: 293655
1965
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Abstract
Six subfacies of the granulite facies are based on variable load pressure, water-vapor pressure, and temperature. Two subfacies of relatively high load pressure are characterized by clinopyroxene-almandite, two intermediate subfacies by orthopyroxene-plagioclase, and two subfacies of relatively low load pressure by cordierite-almandite assemblages in rocks with excess silica. Three subfacies with relatively high water-vapor pressure contain hornblende or biotite, or both, in addition to the characteristic anhydrous assemblages of three subfacies of relatively low water-vapor pressure.
| Reference Key |
openalex_W2318090806
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| Authors | D. deWaard |
| Journal | american journal of science |
| Year | 1965 |
| DOI |
10.2475/ajs.263.5.455
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| URL | |
| Keywords | Keywords not found |
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