supported by the National Natural Science Foundation of China (Nos.41172202,41190073,and 41402075);the China Geological Survey (No.1212011121256);the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan (No.MSFGPMR201502)
The Openness based on DEM emphasizes the terrain convexity and concavity. It facilitates the interpretation of detailed landforms on the Earth's surface. Compared with the layer stacking of ETM+ with less three-dime...
financial supports by the National Natural Science Foundation of China(Nos.41490613,41190073 and 41304071);the National Basic Research Program of China(Nos.2014CB440901 and 2015CB856106)
2D thermo-mechanical models are constructed to investigate the effects of oceanic and continental crustal eclogitization on plate dynamics at three successive stages of oceanic subduction, slab breakoff, and continent...
supported by the NSFC(Nos.41172202 and 41190073);the China Geological Survey(No.1212011121256);the Ministry of Education of China(No.20110145130001);the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences in Wuhan(No.MSFGPMR201402)
Zircon U-Pb dating, Lu-Hf isotopic and geochemical data for the Silurian rhyolites from the Loei fold belt are presented to constrain their petrogenesis and tectonic settings. The rhyolites give a weighted mean 206Pb/...
supported by the National Natural Science Foundation of China (Nos. 41172202, 41190073);the China Geological Survey (No. 1212011121256);the State Key Laboratory of Geological Processes and Mineral Resources, China Uni-versity of Geosciences in Wuhan (No. MSFGPMR201402)
The Changning-Menglian belt, distributed over southwestern Yunnan Province in Southwest China, contains oceanic rocks that are considered to be remnants of the Paleotethys. This study observed Triassic siliceous rocks...
supported by the National Natural Science Foundationof China(No.41190073);the National Basic Research Program of China(No.2014CB440901);the Fundamental Research Funds for the Central Universities to SYSU
The Wuliangshan Group occurs to the east of the Lancang giant igneous zone in SW Yunnan, and is mainly composed of low-grade metamorphosed sedimentary rocks. The group has been considered as the syn-orogenic product o...
Supported by the National Basic Research Program of China(No.2014CB440901);the China National Natural Science Foundation(No.41190073);the Fundamental Research Funds for the Central Universities to SYSU
The Ailaoshan-Red River(ASRR) shear zone in SW China represents an important discontinuity believed to have accommodated eastward extrusion of the Tibetan Plateau in response to the collision of the Indian and Euras...