FEATURES OF GEOLOGICAL STRUCTURE AND PETROGRAPHIC COMPOSITION OF JIL-QARAKHACH HYPERBASITE PROTRUSIVE MASSIF OF SEVAN–HAKARI OPHIOLITE ZONE

Authors

  • H.P. Guyumjyan Chair of Regional Geology and Minerals Survey, YSU, Armenia
  • Sh.V. Khachatryan Chair of Regional Geology and Minerals Survey, YSU, Armenia

DOI:

https://doi.org/10.46991/PYSU:C/2016.50.2.003

Keywords:

Jil-Qarakhach protrusive massif, hyperbasite, tectonic contact, Sevan–Hakari ophiolite zone

Abstract

The processes that lead to the introduction of ophiolites, it is much easier to associate with the displaced protrusions on deep faults, than with the magmatic intrusion (according to classical concepts) or obduction mechanism (under-hypothes of plate tectonics). The tectonic nature of the contact zone of hyperbasites and limestones (where rocks are deformed, brecciated and mylonitied) and the lack of high-temperature contact metamorphism around ophiolites massif are shown. In addition the article presents the petrographic characteristics of hyperbasites.

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Published

2016-08-15

How to Cite

Guyumjyan, H., & Khachatryan, S. (2016). FEATURES OF GEOLOGICAL STRUCTURE AND PETROGRAPHIC COMPOSITION OF JIL-QARAKHACH HYPERBASITE PROTRUSIVE MASSIF OF SEVAN–HAKARI OPHIOLITE ZONE. Proceedings of the YSU C: Geological and Geographical Sciences, 50(2 (240), 3–13. https://doi.org/10.46991/PYSU:C/2016.50.2.003

Issue

Vol. 50 No. 2 (240) (2016)

Section

Geology

License

Copyright (c) 2016 Proceedings of the YSU

Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.

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