ИСЛАНД УЛСЫН БАГА ТЕМПЕРАТУРТАЙ, ГАЗРЫН ГҮНИЙ ДУЛААНЫ ИЛЭРЦТЭЙ ТАЛБАЙ ДЭЭРХ ТЕМ БА МТ АРГУУДЫН ХЭРЭГЛЭЭ

Authors

  • Саранцэцэг Л Одон Орон Геофизикийн Хүрээлэн, ШУА, Монгол улс
  • Hersir P G Iceland Geosurvey-ISOR
  • Arnason К Iceland Geosurvey-ISOR

Keywords:

geothermal, resistivity, magnetotellurics

Abstract

Geothermal exploration involves geology, geochemistry and geophysics. In geophysical exploration, resistivity surveying plays a most important role in delineating the reservoir. The parameters that control the geothermal system show a strong response to electrical resistivity. The resistivity methods that are mostly used in geothermal exploration in Iceland are TEM (Transient electromagnetics) and MT (Magnetotellurics). The resulting resistivity cross sections and resistivity depth slices, show a shallow lying low resistivity layer and deep lying low resistivity towards the end of the cross sections
Abstract
2069
PDF
2270

Downloads

Published

2017-08-15

How to Cite

ИСЛАНД УЛСЫН БАГА ТЕМПЕРАТУРТАЙ, ГАЗРЫН ГҮНИЙ ДУЛААНЫ ИЛЭРЦТЭЙ ТАЛБАЙ ДЭЭРХ ТЕМ БА МТ АРГУУДЫН ХЭРЭГЛЭЭ. (2017). Proceedings of the Mongolian Academy of Sciences, 57(2), 24-33. https://doi.org/10.5564/pmas.v57i2.849

Issue

Vol. 57 No 02(222) 2017

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.

How to Cite

ИСЛАНД УЛСЫН БАГА ТЕМПЕРАТУРТАЙ, ГАЗРЫН ГҮНИЙ ДУЛААНЫ ИЛЭРЦТЭЙ ТАЛБАЙ ДЭЭРХ ТЕМ БА МТ АРГУУДЫН ХЭРЭГЛЭЭ. (2017). Proceedings of the Mongolian Academy of Sciences, 57(2), 24-33. https://doi.org/10.5564/pmas.v57i2.849