Partitioning of Fe (super ++) and Mg (super ++) between coexisting synthetic olivine and orthopyroxene

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ID: 293564
1969
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Abstract
Partitioning curves, experimental procedures and results, comparison with compositions, index of equilibria, absence of temperature dependence, application of data to pairs from chrondritic meteorites, stratiform basic intrusions, peridotite nodules, and alpine peridotites
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openalex_W2313757888 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors L. Gordon Medaris
Journal american journal of science
Year 1969
DOI
10.2475/ajs.267.8.945
URL
Keywords Keywords not found

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