Mechanisms to generate ultrahigh-temperature metamorphism
Ultrahigh-temperature (UHT; T max≥ 900° C) metamorphism requires unusually high heat
in continental crust at depths of 15–55 km, but how such extreme thermal conditions are …
in continental crust at depths of 15–55 km, but how such extreme thermal conditions are …
Subduction initiation triggered by collision: A review based on examples and models
G Yang - Earth-Science Reviews, 2022 - Elsevier
Subduction initiation is one of the main unsolved issues in plate tectonics theory with
different proposed mechanisms. In the arc (plateau, terrane)-continent collision models, a …
different proposed mechanisms. In the arc (plateau, terrane)-continent collision models, a …
Discovery and genesis of helium-rich geothermal fluids along the India–Asia continental convergent margin
Large-scale helium accumulations are rarely reported in tectonically active continental
subduction zones. This study shows geochemical variations in helium and other volatiles (N …
subduction zones. This study shows geochemical variations in helium and other volatiles (N …
Magmatic fluid input controlling the geochemical and isotopic characteristics of geothermal waters along the Yadong-Gulu rift, southern Tibetan Plateau
Geothermal resources, regarded as sustainable green energy, are attracting increasing
attention. The southern Tibetan Plateau possesses the most abundant intermediate-high …
attention. The southern Tibetan Plateau possesses the most abundant intermediate-high …
Organic and inorganic carbon sinks reduce long‐term deep carbon emissions in the continental collision margin of the southern Tibetan Plateau: Implications for …
This paper aims to update our understanding of the carbon cycle in the Himalayas, the most
intense collisional orogeny globally, by providing new insight into its impact on Cenozoic …
intense collisional orogeny globally, by providing new insight into its impact on Cenozoic …
Gas geochemical evidence for the India-Asia lithospheric transition boundary near the Karakorum fault in western Tibet
The lithospheric structure of the Tibetan Plateau plays a key role in explaining the
underlying plateau formation mechanism (s) and growth history. Although many studies …
underlying plateau formation mechanism (s) and growth history. Although many studies …
Streamflow composition and water “imbalance” in the northern Himalayas
Abstract The Yarlung Zangbo River (YZR) is the largest river in the northern Himalayas,
providing crucial water resources for downstream. A full understanding of the streamflow …
providing crucial water resources for downstream. A full understanding of the streamflow …
Subducting Indian lithosphere controls the deep carbon emission in Lhasa terrane, southern Tibet
Abstract The India‐Asia orogenic zone is considered to participate significantly in the Earth's
geological carbon budget. However, the carbon cycling process at orogenic belts with …
geological carbon budget. However, the carbon cycling process at orogenic belts with …
Hydrothermal He and CO2 degassing from a Y-shaped active fault system in eastern Tibetan Plateau with implications for seismogenic processes
Degassing of deeply-derived fluids (eg, He and CO 2) prevails along seismically active
faults in continental collision settings such as the Tibetan Plateau, where potential insights …
faults in continental collision settings such as the Tibetan Plateau, where potential insights …
Hydrogeochemical characterization and precursor anomalies of hot springs in the North Tianshan orogen
Z Ding, X Zhou, C Wang, J Li, M He, J Tian… - Applied …, 2023 - Elsevier
Abstract The North Tianshan orogen consists of a series of thrust faults and is the most
seismic region in China. In this paper, the characteristics of hot springs in the North …
seismic region in China. In this paper, the characteristics of hot springs in the North …