Stable isotopes (δ 13 C DIC , δD, δ 18 O) and geochemical characteristics of geothermal springs of Ladakh and Himachal (India): Evidence for CO 2 discharge in northwest Himalaya-Reference-Cited by-同舟云学术

Stable isotopes (δ 13 C DIC , δD, δ 18 O) and geochemical characteristics of geothermal springs of Ladakh and Himachal (India): Evidence for CO 2 discharge in northwest Himalaya

Published:2016-11 Issue: Volume:64 Page:314-330
ISSN:0375-6505
Container-title:Geothermics
language:en
Short-container-title:Geothermics

Author:

Tiwari Sameer K.,Rai Santosh K.,Bartarya Sukesh K.,Gupta Anil K.,Negi Manju

Funder

Department of Science and Technology (DST), Government of India

Publisher

Elsevier BV

Subject

Geology,Geotechnical Engineering and Engineering Geology,Renewable Energy, Sustainability and the Environment

Reference75 articles.

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3. Magnetotelluric evidence of potential geothermal resource in Puga, Ladakh, NW Himalaya;Azeez;Curr. Geosci.,2007

4. Global Distribution of Carbon Dioxide Discharges and Major Zones of Seismicity;Barnes,1986

5. δ18O and δD systematics in the surficial waters of the Gaula river catchment area, Kumaun Himalaya, India;Bartarya;J. Hydrol.,1995

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