Special Features of the Forming of Thermal Waters of the Eastern Part of the Khangay Neotectonic Uplift

Authors

  • PS Badminov Institute of the earth’s crust, RAS
  • D Ganchimeg Institute of chemistry and chemical technology, MAS
  • BI Pisarsky Institute of the earth’s crust, RAS
  • D Oyuntsetseg Institute of chemistry and chemical technology, MAS
  • GI Orgilyanov Institute of the earth’s crust, RAS
  • IG Kryukova Institute of the earth’s crust, RAS
  • Ch Zundui-Osor Mega Watt Co. Ltd

DOI:

https://doi.org/10.5564/pmas.v0i4.48

Keywords:

thermal waters, Khangay

Abstract

Khangay neotectonic uplift is a large block of the earth’s crust confined to the area between two sublatitudinal deep faults (Bulnay and Goby-Altay). They are active faults accommodating main compression stresses in contract to the extension existed in the other area of the Khangay uplift. In contrast to continental rift zones of Khangay it is the region of compression. It is area with the increased values of the heat flux.

DOI: http://dx.doi.org/10.5564/pmas.v0i4.48

Proceedings of the Mongolian Academy of Sciences 2009 No 4 pp.64-70

Downloads

Download data is not yet available.
Abstract
1757
PDF
1748

Downloads

Published

2011-03-18

How to Cite

Badminov, P., Ganchimeg, D., Pisarsky, B., Oyuntsetseg, D., Orgilyanov, G., Kryukova, I., & Zundui-Osor, C. (2011). Special Features of the Forming of Thermal Waters of the Eastern Part of the Khangay Neotectonic Uplift. Proceedings of the Mongolian Academy of Sciences, 49(4), 64–70. https://doi.org/10.5564/pmas.v0i4.48

Issue

Vol. 49 No 04(194) 2009

Section

Articles

License

Copyright on any research article in the Proceedings of the Mongolian Academy of Sciences is retained by the author(s).

The authors grant the Proceedings of the Mongolian Academy of Sciences a license to publish the article and identify itself as the original publisher.

Creative Commons Licence
Articles in the Proceedings of the Mongolian Academy of Sciences are Open Access articles published under a Creative Commons Attribution 4.0 International License CC BY.

This license permits use, distribution and reproduction in any medium, provided the original work is properly cited.