Junfeng Gong
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View article: Uplift History of the Eastern Pamir Inferred from Inversion of Thermochronometric Data and River Profile
Uplift History of the Eastern Pamir Inferred from Inversion of Thermochronometric Data and River Profile Open
The Pamir salient accommodates a great amount of Cenozoic India-Eurasia convergence in the forms of thrusting, strike-slip faulting, extension, and gneiss dome formation. It thus becomes a key location for exploring the orogenic tectonic e…
View article: Westward Migration of the Chenghai–Jinsha Drainage Divide and Its Implication for the Initiation of the Chenghai Fault
Westward Migration of the Chenghai–Jinsha Drainage Divide and Its Implication for the Initiation of the Chenghai Fault Open
The Chenghai Fault in the Chuan–Dian block terminates at the northwestern segment of the Red River Fault, and is a significant seismogenic structure. The kinematic evolution of this fault should be closely related to the regional tectonic …
View article: Gneiss dome exhumation aided by extrusion along a step-form detachment in the Eastern Pamir
Gneiss dome exhumation aided by extrusion along a step-form detachment in the Eastern Pamir Open
Supplementary data for submission "Gneiss dome exhumation aided by extrusion along a step-form detachment in the Eastern Pamir" to G-cubed.
View article: Gneiss dome exhumation aided by extrusion along a step-form detachment in the Eastern Pamir
Gneiss dome exhumation aided by extrusion along a step-form detachment in the Eastern Pamir Open
Supplementary data for submission "Gneiss dome exhumation aided by extrusion along a step-form detachment in the Eastern Pamir" to G-cubed.
View article: “V”型共轭走滑断裂：特征、形成机制及其对青藏高原东南缘晚新生代变形的启示
“V”型共轭走滑断裂：特征、形成机制及其对青藏高原东南缘晚新生代变形的启示 Open
摘要: "V"型共轭走滑断裂是指共轭角为钝角的共轭走滑断裂,其"V"型开口方向为锐角且指示最大拉伸方向.前人开展了大量关于"V"型共轭走滑断裂发育背景及动力学机制的研究,但是目前未有针对"V"型共轭断裂几何学、运动学有关的综述.归纳已有"V"型共轭走滑断裂的几何学、运动学特征,总结现存的"V"型共轭走滑断裂的动力学机制,并选取青藏高原东南缘"V"型共轭走滑断裂,进行实例分析.分布于美国西部、欧亚板块中西部和西藏中部的"V"型共轭走滑断裂特征揭示共轭角大小与断裂滑动速率及断裂…
View article: Evolution of the Yangtze River network, southeastern Tibet: Insights from thermochronology and sedimentology
Evolution of the Yangtze River network, southeastern Tibet: Insights from thermochronology and sedimentology Open
We performed apatite and zircon (U-Th)/He dating on a granitic pluton that has been offset by ∼10 km by motion on the sinistral strike-slip Xiangcheng fault in SW Sichuan, SE Tibetan plateau, where the Shuoqu River incises a deep valley be…
View article: Early Pleistocene drainage pattern changes in Eastern Tibet: Constraints from provenance analysis, thermochronometry, and numerical modeling
Early Pleistocene drainage pattern changes in Eastern Tibet: Constraints from provenance analysis, thermochronometry, and numerical modeling Open
The geometry and evolution of fluvial systems are thought to be related to surface uplift. In eastern Tibet, rivers exhibit peculiar drainage patterns but how these patterns were established and their connection with the plateau uplift are…