ORIGIN OF TOURMALINE GRANITOIDS OF MEGHRI PLUTON'S VANK INTRUSIVE MASSIVE
DOI:
https://doi.org/10.46991/PYSU:C/2015.49.2.009Keywords:
tourmaline granitoids, borates, magmatic genesis of tourmalineAbstract
In the Vank granitoids turmalin is spread unevenly regardless of magmatic and tectonic cracks. The three types of turmaline: magmatic (porphyric inclusions in the granitoids), pneumatolytic (radial-rays aggregates in the andesits at the top of Vank's massive) and hydrothermal (quartz-turmaline veins in the exocontact gabbros and monzonite), are genetically associated with magmatic and post magmatic processes of the boron enriched Vank's intrusive.
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Published
2015-08-10
How to Cite
Guyumjyan, H. (2015). ORIGIN OF TOURMALINE GRANITOIDS OF MEGHRI PLUTON’S VANK INTRUSIVE MASSIVE. Proceedings of the YSU C: Geological and Geographical Sciences, 49(2 (237), 9–15. https://doi.org/10.46991/PYSU:C/2015.49.2.009
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Geology
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