Formation of giant copper deposits in Tibet driven by tearing of the subducted Indian plate
Porphyry copper deposits (PCDs) occur in accretionary and collisional orogens, yet it is
unclear how continental collision controls their formation. Two fundamental issues are …
unclear how continental collision controls their formation. Two fundamental issues are …
Porphyry mineralization in the Tethyan orogen
The Tethyan metallogenic domain (TMD), as one of the three major domains in the world,
extends over 10000 km from east to west, and has developed several world-class …
extends over 10000 km from east to west, and has developed several world-class …
USTClitho2. 0: Updated unified seismic tomography models for Continental China lithosphere from joint inversion of body‐wave arrival times and surface‐wave …
Abstract presented 3D seismic velocity models (VP and VS) of crust and uppermost mantle
of continental China using seismic body‐wave travel‐time tomography, which are referred to …
of continental China using seismic body‐wave travel‐time tomography, which are referred to …
Refertilized continental root controls the formation of the Mianning–Dechang carbonatite-associated rare-earth-element ore system
Rare earth element ore deposits associated with carbonatite derived from Earth's mantle
supply half of the world's rare earth element. However, the formation of carbonatite and …
supply half of the world's rare earth element. However, the formation of carbonatite and …
The impact of a tear in the subducted Indian plate on the Miocene geology of the Himalayan-Tibetan orogen
Abstract The Yadong-Gulu Rift, cutting across the Gangdese belt and Himalayan terranes, is
currently associated with a thermal anomaly in the mantle and crustal melting at 15–20 km …
currently associated with a thermal anomaly in the mantle and crustal melting at 15–20 km …
Three-dimensional kinematics of the India–Eurasia collision
L Wang, S Barbot - Communications Earth & Environment, 2023 - nature.com
The collision between India and Eurasia mobilizes multiple processes of continental
tectonics. However, how deformation develops within the lithosphere across the Tibetan …
tectonics. However, how deformation develops within the lithosphere across the Tibetan …
Relationship of the crustal structure, rheology, and tectonic dynamics beneath the Lhasa‐Gangdese terrane (southern Tibet) based on a 3‐D electrical model
The tectonic dynamics of the Lhasa‐Gangdese terrane, southern Tibet, are still unclear and
open questions persist regarding the structure, physical properties, and rheology of the …
open questions persist regarding the structure, physical properties, and rheology of the …
[HTML][HTML] 青藏高原近南北向裂谷的时空分布特征及动力学机制
卞爽， 于志泉， 龚俊峰， 杨蓉， 程晓敢， 林秀斌… - 地质力学 …, 2021 - journal.geomech.ac.cn
青藏高原南部发育的一系列近南北向裂谷是印度-欧亚大陆持续挤压作用下的大型伸展构造,
也是揭示高原后碰撞构造演化过程的重要对象. 目前, 关于南北向裂谷的形成机制存在多种假说 …
也是揭示高原后碰撞构造演化过程的重要对象. 目前, 关于南北向裂谷的形成机制存在多种假说 …
Along‐strike variation in the initiation timing of the north‐trending rifts in southern Tibet as revealed from the Yadong‐Gulu rift
A key issue in the Cenozoic evolution of the Tibetan plateau is the geodynamic drivers for
north‐trending rifting in southern Tibet. Recent studies have demonstrated an eastward …
north‐trending rifting in southern Tibet. Recent studies have demonstrated an eastward …
Deformation of crust and upper mantle in central Tibet caused by the northward subduction and slab tearing of the Indian lithosphere: New evidence based on shear …
Shear-wave splitting provides insight into geodynamic processes such as lithospheric
deformation and upper mantle flow. This study presents shear wave splitting parameters …
deformation and upper mantle flow. This study presents shear wave splitting parameters …