Tracing the evolution of shallow geothermal springs in the Shyok−Nubra Valley of North-West Himalayas, India through hydrogeochemistry and stable isotopes (δ18O, δD)-Reference-Cited by-同舟云学术

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Tracing the evolution of shallow geothermal springs in the Shyok−Nubra Valley of North-West Himalayas, India through hydrogeochemistry and stable isotopes (δ18O, δD)

Published:2024-06 Issue:2 Volume:9 Page:100175
ISSN:2451-912X
Container-title:Solid Earth Sciences
language:en
Short-container-title:Solid Earth Sciences

Author:

Mishra Parashar,Dutta Archisman^ORCID,Absar Ahsan,Malviya Vivek Prakash^ORCID,Saini Pankaj,Thapliyal Ayodhaya Prasad,Banerjee Sayandeep

Funder

Banaras Hindu University

Chinese Academy of Sciences

GSI Helmholtzzentrum für Schwerionenforschung

Publisher

Elsevier BV

Reference70 articles.

1. Report on Puga-Chumathang Geothermal Exploration Project;Absar,1981

2. A preliminary conceptual model of Nubra valley geothermal system, Ladakh, J & K, India;Absar;Geol. Soc. India,1991

3. Genetic aspects of the Puga geothermal system, District Leh, Ladakh, in the light of geological, geophysical and geochemical characteristics. Gond;Absar;Geol. Soc. Sp. Pub.,2023

4. Standard Methods for the Examination of Water and Waste Water,1985

5. The use of mixing models and chemical geothermometers for estimating underground temperatures in geothermal systems;Arnórsson;J. Volcanol. Geotherm. Res.,1985

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