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Uplift of the West Kunlun Range, northern Tibetan Plateau, dominated by brittle thickening of the up
Geochemistry, zircon U/Pb geochronology and Lu\Hf isotopic composition of eclogites and their host g
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Eocene high grade metamorphism and crustal anatexis in the North Himalaya Gneiss Domes, Southern Tib
Rock Damage Structure of the South Longmen-Shan Fault in the 2008 M8 Wenchuan Earthquake Viewed with
Petrogenesis of Miocene adakitic diorite-porphyrite in middle Gangdese batholith, southern Tibet: Co
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Reworking of the Gangdese magmatic arc, southeastern Tibet: post-collisional metamorphism and anatex
The Mesozoic metamorphic–magmatic events in the Medog area, the Eastern Himalayan Syntaxis: constrai
Diamonds, native elements and metal alloys from chromitites of the Ray-Izophiolite of the Polar Ural
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Precambrian evolution of the Lhasa terrane, Tibet: Constraint fromthe zircon U–Pb geochronology of t
Cambrian ultrapotassic rhyolites from the Lhasa terrane, south Tibet: Evidence for Andean-type magma
Early-Neoproterozoic Grenvillian orogeny in Altun-Qilian -North Qaidam, North Tibet: new geochemical
Orogen-parallel ductile extension and extrusion of the Greater Himalaya in the late Oligocene and Mi
Lithospheric Architecture of the Lhasa Terrane and Its Control on Ore Deposits in the Himalayan-Tibe
A genetic linkage between subduction- and collision-related porphyry Cu deposits in continental coll
Late Quaternary slip-rate along the central Bangong-Chaxikang segment of the Karakorum fault, wester
Long-term temperature records following the Mw 7.9 Wenchuan (China) earthquake are consistent with l
Multiple generations of pseudotachylyte in the Wenchuan fault zone and their implications for coseis
Iron isotope evidence for multistage melt–peridotite interactions in the lithospheric mantle of east
Multiple metamorphic events revealed by zircons from the Diancang Shan-Ailao Shan metamorphic comple
Kinematics of the Tengchong Terrane in SE Tibet from the late Eocene to early Miocene: Insights from
Tectonic framework and crustal evolution of the Precambrian basement of the Tarim Block in NW China:
Formation of carbonatite-related giant rare-earth-element deposits by the recycling of marine sedime
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