Fluid geochemistry and its implications on the role of deep faults in the genesis of high temperature systems in the eastern edge of the Qinghai Tibet Plateau
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Title
Fluid geochemistry and its implications on the role of deep faults in the genesis of high temperature systems in the eastern edge of the Qinghai Tibet Plateau
Authors
Keywords
Qinghai-tibet plateau, Longmenshan fault, Xianshuihe fault, High-temperature geothermal system, Geothermal fluid
Journal
APPLIED GEOCHEMISTRY
Volume 131, Issue -, Pages 105036
Publisher
Elsevier BV
Online
2021-06-24
DOI
10.1016/j.apgeochem.2021.105036
References
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Related references
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- Crustal structure across the NE Tibetan Plateau and Ordos Block from the joint inversion of receiver functions and Rayleigh-wave dispersions
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- (2016) Xianchun Tang et al. Environmental Earth Sciences
- Propagation of the deformation and growth of the Tibetan–Himalayan orogen: A review
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- Travertine deposits, deep thermal metamorphism and tectonic activity in the Longmenshan tectonic region, southwestern China
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- Temperature beneath Tibet
- (2013) Chi-yuen Wang et al. EARTH AND PLANETARY SCIENCE LETTERS
- Crustal structure across the Kunlun fault from passive source seismic profiling in East Tibet
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- Geochemistry of soil gas in the seismic fault zone produced by the Wenchuan Ms 8.0 earthquake, southwestern China
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- Crustal deformation of the eastern Tibetan plateau revealed by magnetotelluric imaging
- (2010) Denghai Bai et al. Nature Geoscience
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