Magmatic fluid input explaining the geochemical anomaly of very high arsenic in some southern Tibetan geothermal waters-Reference-Cited by-同舟云学术

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Magmatic fluid input explaining the geochemical anomaly of very high arsenic in some southern Tibetan geothermal waters

Published:2019-05 Issue: Volume:513 Page:32-43
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Guo Qinghai,Planer-Friedrich Britta,Liu Mingliang,Yan Ketao,Wu Geng

Funder

National Natural Science Foundation of China

Fundamental Research Funds for the Central Universities

China University of Geosciences, Wuhan

German Research Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference103 articles.

1. Magnetotelluric images of deep crustal structure of the Rehai geothermal field near Tengchong, southern China;Bai;Geophys. J. Int.,2001

2. Geological features of Larderello-Travale and Mt. Amiata geothermal areas (southern Tuscany, Italy);Batini;Episodes,2003

3. Chloride and Boron behavior in fluids of Los Humeros geothermal field (Mexico): a model based on the existence of deep acid brine;Bernard;Appl. Geochem.,2011

4. The origin of reservoir fluids in the geothermal field of Los Azufres, Mexico — isotopical and hydrological indications;Birkle;Appl. Geochem.,2002

5. Mechanisms of arsenic enrichment in geothermal and petroleum reservoirs fluids in Mexico;Birkle;Water Res.,2010

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