ORE KNOT OF SHNOGH-KOGHB

Authors

  • H. A. Tumanyan Institute of Geological Sciences of the NAS of RA, Armenia
  • R. S. Movsesyan Chair of Regional Geology and Minerals Survey, YSU, Armenia
  • H. I. Movsisyan Chair of Regional Geology and Minerals Survey, YSU, Armenia

DOI:

https://doi.org/10.46991/PYSU:C/2009.43.2.013

Keywords:

ore knot of Shnogh-Koghb, upper mantle-crust, zone of hydrothermal-metasomatic transformed rocks, aerospacedistanced datа, geophysical and geochemical anomalies

Abstract

The ore knot is placed on crossing through upper mantle-crust NE and crust NW breaks, where the magmatic formations are intensively shown in different depths of formation, field and zone of hydrothermal-metasomatic transformed rocks, endogenous ore accumulation. It is distinguished by geological-structural, aerospacedistanced datа, local geophysical and geochemical anomalies.

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Published

2009-07-13

How to Cite

Tumanyan, H. A., Movsesyan, R. S., & Movsisyan, H. I. (2009). ORE KNOT OF SHNOGH-KOGHB. Proceedings of the YSU C: Geological and Geographical Sciences, 43(2 (219), 13–21. https://doi.org/10.46991/PYSU:C/2009.43.2.013

Issue

Vol. 43 No. 2 (219) (2009)

Section

Geology

License

Copyright (c) 2009 Proceedings of the YSU

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