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Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures
Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on
earth, and become a key region for comprehending the rheology and tectonic evolution of …
earth, and become a key region for comprehending the rheology and tectonic evolution of …
[HTML][HTML] Crustal conductivity footprint of the Miocene porphyry copper polymetallic deposits in the Gangdese metallogenic belt, Tibetan Plateau
New evidence worldwide has linked the surface locations of mineral deposits and their
crustal-scale electrical conductivity footprint. We examine the relationship between the …
crustal-scale electrical conductivity footprint. We examine the relationship between the …
Different formation modes of the north–south‐trending rifts in southern Tibet: Implications from ambient noise tomography
Understanding how the Miocene N–S‐trending rifts on the southern Tibetan Plateau formed
is crucial for understanding the evolution of the plateau. Most competing models suggest …
is crucial for understanding the evolution of the plateau. Most competing models suggest …
[HTML][HTML] Evidence for partial melting and alkali-rich fluids in the crust from a 3-D electrical resistivity model in the vicinity of the Coqen region, western Lhasa terrane …
Both low resistivity zones and low velocity zones are distributed in the middle-lower crust of
the western Lhasa terrane, Tibetan Plateau, China. Some estimates from electrical resistivity …
the western Lhasa terrane, Tibetan Plateau, China. Some estimates from electrical resistivity …
Crustal melting and continent uplift by mafic underplating at convergent boundaries
The thick crust of the southern Tibetan and central Andean plateaus includes high-
conductivity, low-velocity zones ascribed to partial melt. The melt origin and effect on plateau …
conductivity, low-velocity zones ascribed to partial melt. The melt origin and effect on plateau …
Indian Crustal Front beneath Tibet Inferred from Seismic Anisotropy
Postcollisional downgoing of the Indian plate has absorbed large amounts of the Cenozoic
India–Asia convergence and is a key process governing the Tibetan Plateau's evolution and …
India–Asia convergence and is a key process governing the Tibetan Plateau's evolution and …
[HTML][HTML] The structure of a continental intraplate volcanic system and controls from shear zones: Insights into the central Hoggar Cenozoic volcanic province …
Continental intraplate volcanic systems, with their locations far from plate tectonic
boundaries, are not well understood: the crustal and lithospheric mantle structure of these …
boundaries, are not well understood: the crustal and lithospheric mantle structure of these …
[HTML][HTML] Lithium isotopes in the geothermal waters of the Indian–Asian continental convergent margin: Source and evolution
Lithium (Li) in geothermal waters along the Indian–Asian continental convergent margin is a
potential Li resource and plays an important role in the Li budget and Li isotopic composition …
potential Li resource and plays an important role in the Li budget and Li isotopic composition …
Isolated crustal partial melting in the southern Tibetan Plateau from H‐κ‐c method
The crustal thickness and average Vp/Vs ratio are basic parameters to understand the
current state and the tectonic processes in the Tibetan Plateau (TP). We gather receiver …
current state and the tectonic processes in the Tibetan Plateau (TP). We gather receiver …
Relationship between the migration of crustal material, normal faulting, and gneiss domes in the vicinity of the dinggye region, Central part of the tethys–Himalaya …
The Dinggye region, in the central part of the Himalayan orogenic belt, includes the southern
part of the Xainza-Dinggye rift and the Mabja Gneiss Dome with leucogranite cores …
part of the Xainza-Dinggye rift and the Mabja Gneiss Dome with leucogranite cores …