KEY FEATURES OF GEOLOGICAL STRUCTURE OF BARTSRAVAN ORE FIELD AND THE RESULTS OF GEOPHYSICAL RESEARCH

Authors

  • H. P. Guyumjyan Chair of Mineralogy, Petrology and Geochemistry, YSU, Armenia
  • G. V. Markosyan Chair of Geophysics, YSU, Armenia
  • S. V. Voskanyan Chair of Historical and Regional Geology, YSU, Armenia

DOI:

https://doi.org/10.46991/PYSU:C/2012.46.3.003

Keywords:

mineralization, stratigraphy, volcanism, magnetic prospecting, electrical prospecting

Abstract

In geological structure of Bardzravan ore field the main role belongs to the volcanic-sedimentary formations of the lower and middle Eocene. These rocks are covered unconformably with lava and pyroclastic formations of salvard suit of the middle-upper Miocene. Metasomatic rocks, which confined to the gold-bearing, are widely distributed within the ore field. The article also presents the data of geophysical studies, which were made in the central part of the ore field.

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Published

2012-12-10

How to Cite

Guyumjyan, H. P., Markosyan, G. V., & Voskanyan, S. V. (2012). KEY FEATURES OF GEOLOGICAL STRUCTURE OF BARTSRAVAN ORE FIELD AND THE RESULTS OF GEOPHYSICAL RESEARCH. Proceedings of the YSU C: Geological and Geographical Sciences, 46(3 (229), 3–10. https://doi.org/10.46991/PYSU:C/2012.46.3.003

Issue

Vol. 46 No. 3 (229) (2012)

Section

Geology

License

Copyright (c) 2012 Proceedings of the YSU

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