Enlargement of the composition field of epidote and piemontite with rising temperature

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ID: 294213
1958
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Abstract
"At very low temperatures, epidote and piemontite tend to have compositions near HCa 2 Al 2 FeSi 3 O 13 . With rising temperature, the composition field of these minerals enlarges toward higher and lower Fe (super +3) contents and also toward higher Mn (super +3) content."
Reference Key
openalex_W2327694683 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors A. Miyashiro, Yuya Seki
Journal american journal of science
Year 1958
DOI
10.2475/ajs.256.6.423
URL
https://doi.org/10.2475/ajs.256.6.423
Keywords Keywords not found

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