Chemical and isotopic constraints on fluid origin and genesis of geothermal systems in the Tingri-Tangra Yumco rift, southern Tibetan Plateau

Chemical and isotopic constraints on fluid origin and genesis of geothermal systems in the Tingri-Tangra Yumco rift, southern Tibetan Plateau

Abstract Numerous geothermal systems are hosted by extensional rifts that transect the Himalayas and Lhasa block in the Himalayan–Tibetan orogen. However, the relationships between hydrogeological processes and geothermal fluid circulation in different tectonic units remain unclear. Here, we report...

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Bibliographic Details
Main Authors: Wei Liu, Maoliang Zhang, Yi Liu, Lifeng Cui, Yuji Sano, Sheng Xu
Format: Article
Language:English
Published: SpringerOpen 2024-09-01
Series:Geothermal Energy
Subjects:
Geothermal fluids
Hydrochemistry
Stable isotopes
Geothermometry
Tingri-Tangra Yumco rift
Himalayan–Tibetan orogen
Online Access:https://doi.org/10.1186/s40517-024-00311-8

Internet

https://doi.org/10.1186/s40517-024-00311-8

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