O, H, and Sr isotope evidence for origin and mixing processes of the Gudui geothermal system, Himalayas, China

Volume: 11, Issue: 4, Pages: 1175 - 1187
Published: Jul 1, 2020
Abstract
The Gudui geothermal field records the highest temperature at equivalent borehole depths among the mainland hydrothermal systems in mainland China. Located about 150 ​km southeast of Lhasa City, the capital of Tibet, the Gudui geothermal field belongs to the Sangri–Cuona rift belt, also known as the Sangri–Cuona geothermal belt, and is representative of the non-volcanic geothermal systems in the Himalayas. In this study, oxygen-18 and deuterium...
Paper Details
Title
O, H, and Sr isotope evidence for origin and mixing processes of the Gudui geothermal system, Himalayas, China
Published Date
Jul 1, 2020
Volume
11
Issue
4
Pages
1175 - 1187
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