Sulphur evolution in acidic and alkaline geothermal water related to magma in the Rehai geothermal field in the southeastern Tibet Plateau based on stable hydrogen, oxygen, sulphur isotopes-Reference-Cited by-同舟云学术

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Sulphur evolution in acidic and alkaline geothermal water related to magma in the Rehai geothermal field in the southeastern Tibet Plateau based on stable hydrogen, oxygen, sulphur isotopes

Published:2024-05 Issue: Volume:119 Page:102931
ISSN:0375-6505
Container-title:Geothermics
language:en
Short-container-title:Geothermics

Author:

Li Bo,Kong Qingmin,Liao Fu,Wang Guangcai,Liu Fei,Guo Liang,Liu Chenglong,Shi Zheming

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

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

Reference64 articles.

1. The inference of magmatic heat source beneath the Rehai (hot sea) field of Tengchong from the result of magnetotelluric sounding;Bai;Chin. Sci. Bull.,1994

2. From source to surface: tracking magmatic boron and chlorine input into the geothermal systems of the Taupo volcanic zone, New Zealand;Begue;J. Volcanol. Geotherm. Res.,2017

3. Biogeochemistry and bacteriology of ferrous iron oxidation in geothermal habitats;Brock;Geochim. Cosmochim. Acta,1976

4. Sulphur isotope composition of orogenic spinel lherzolite massifs from Ariege (North-Eastern Pyrenees, France): an ion microprobe study;Chaussidon;Geochim. Cosmochim. Acta,1990

5. Oxygen isotope exchange rate between dissolved sulfate andwater at hydrothermal temperatures;Chiba;Geochim. Cosmochim. Acta,1985

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