Metasomatic granitization of batholithic dimensions

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ID: 293670
1949
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Abstract
Discusses synkinematic granitization in the Nanga Parbat area, northwest Himalayas, India, static granitization in the Sheku area, northwest Yunnan, China, and the relationships of synkinematic and static granitization. It is concluded that the majority of large granitic batholiths appear to be of metasomatic origin; that no magmatic source of the agent of large-scale regional granitization is visible within the depths exposed; that the birth of granitization is genetically connected with eugeosynclinal orogeny; that its primary motor is at great depth. In this sense, synkinematic granitization is the original process and static granitization a more secondary consequence, although it is able to rise to higher levels than are generally reached by synkinematic granitization.
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openalex_W2327130500 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Peter Misch
Journal american journal of science
Year 1949
DOI
10.2475/ajs.247.4.209
URL
https://ajsonline.org/article/58201.pdf
Keywords Keywords not found

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