Granitization, metamorphism and volcanism

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ID: 305019
1954
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Abstract
Reaffirms the conclusion that granitization takes place by diffusion in the solid state (introduction of alkalis and removal of Fe and Mg), and discusses the hypothesis that not only granitization but also metamorphism, volcanism, and orogeny may be manifestations of chemical reactions taking place by long-distance diffusion between inner and outer layers of the earth9s crust.
Reference Key
openalex_W2031491561 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Richard K. Perrin
Journal american journal of science
Year 1954
DOI
10.2475/ajs.252.8.449
URL
https://doi.org/10.2475/ajs.252.8.449
Keywords Keywords not found

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