The granites of Trancoso (Portugal); a study in microclinization

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ID: 301196
1956
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Abstract
The increase in microcline content from the center toward the margin of the Trancoso granodiorite massif in north Portugal is considered due to the introduction of potash feldspar material from the surrounding younger porphyritic granite in late stages of its emplacement. The new microcline replaced plagioclase and quartz of the granodiorite, and preexisting microcline was recrystallized.
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openalex_W2325821766 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors L. J. G. Schermerhorn
Journal american journal of science
Year 1956
DOI
10.2475/ajs.254.6.329
URL
https://ajsonline.org/article/58603.pdf
Keywords Keywords not found

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