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.

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

Section

Geology