A petrogenetic grid for the Fe-Mg silicates of pelitic schists

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ID: 293539
1965
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Abstract
The topology of the reaction surfaces for the phases\--garnet, chloritoid, staurolite, kyanite, cordierite, chlorite, and biotite\--is shown for two limiting sections of Ps, T, P ~water~ space. . . . The basic assumption made is that the course of progressive metamorphism is primarily one of progressive dehydration with a progressive restriction of the fields of the most hydrous minerals, notably chlorite. The resulting petrogenetic grids. . . are predominantly theoretical and should serve as a useful check in assigning natural metamorphic sequences to their relative pressure-temperature relationships.
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openalex_W2086180497 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors A. L. Albee
Journal american journal of science
Year 1965
DOI
10.2475/ajs.263.6.512
URL
https://ajs.scholasticahq.com/article/61420.pdf
Keywords Keywords not found

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