A5068218473- Geological and Geochemical Analysis
- earthquake and tectonic studies
- High-pressure geophysics and materials
- Geological and Geophysical Studies
- Geochemistry and Geologic Mapping
- Geochemistry and Geochronology of Asian Mineral Deposits
- Paleontology and Stratigraphy of Fossils
- Geological Studies and Exploration
- Geomagnetism and Paleomagnetism Studies
- Hydrocarbon exploration and reservoir analysis
- Seismic Imaging and Inversion Techniques
- Geology and Paleoclimatology Research
- Paleontology and Evolutionary Biology
- Geochemistry and Elemental Analysis
- Evolution and Paleontology Studies
- Geological and Geophysical Studies Worldwide
- Geophysical and Geoelectrical Methods
- Marine and coastal plant biology
- Rock Mechanics and Modeling
- Geological formations and processes
- Radiomics and Machine Learning in Medical Imaging
- Food Quality and Safety Studies
- Geological Modeling and Analysis
- Geophysics and Gravity Measurements
- Appendicitis Diagnosis and Management
Chinese Academy of Sciences
2015-2024
Institute of Geology and Geophysics
2015-2024
University of Chinese Academy of Sciences
2010-2024
Linyi University
2024
Nanjing Institute of Geology and Paleontology
2011-2023
Czech Academy of Sciences, Institute of Geology
2023
Ethnological Museum
2023
State Key Laboratory of Lithospheric Evolution
2006-2020
Kobe University
2006
Nagoya University
2004-2005
The Trans-North China Belt (TNCB) is a Paleoproterozoic collisional orogen (ca.1.9-1.8Ga) responsible for the amalgamation of North Craton.Detail field works in Lüliangshan, Hengshan, Wutaishan and Fuping massifs where belt well exposed, allow us to draw new tectonic map crustal-scale cross sections.The available petrologic, radiometric, geochronologic data are integrated geodynamic evolution scheme this orogen.The Low Grade Mafic Unit (LGMU) interpreted as an ophiolitic nappe rooted suture...
Abstract In the north‐eastern part of North China Block, a mafic magmatic belt consisting mafic–ultramafic rocks and marine sedimentary crops out between northern Archean Anshan Block southern Palaeoproterozoic Block. 40 Ar/ 39 Ar amphibole ages around 1.9 Ga from gabbros, trace element analyses pyroxenite shale show that these formed along active continental margin. The is interpreted as an arc developed above south‐directed subduction zone, which was subsequently overthrust to north upon...
Research Article| February 01, 2001 Where is the North China–South China block boundary in eastern China? Michel Faure; Faure 1Institut des Sciences de la Terre d'Orléans, Bâtiment Géosciences, Université 45067 Orléans Cedex 2, France Search for other works by this author on: GSW Google Scholar Wei Lin; Lin Nicole Le Breton Geology (2001) 29 (2): 119–122. https://doi.org/10.1130/0091-7613(2001)029<0119:WITNCS>2.0.CO;2 Article history received: 20 Jun 2000 rev-recd: 13 Oct accepted: 26 first...
The Yunkai massif is a key region to decipher the tectonic evolution of south China block since contained high‐grade metamorphic rocks experienced polyphase deformation. earliest event (D 1 ) corresponds top‐to‐the‐northwest ductile shearing, coeval with amphibolite facies metamorphism, probably developed during postorogenic synmigmatization extensional occurred in early Paleozoic time. main deformation 2 top‐to‐the‐northeast Mesozoic time, greenschist metamorphism and associated development...
In the North China block, south Liaodong Peninsula massif is an elliptical metamorphic core complex (MCC) with a long axis trending NE‐SW. cross‐section view, it asymmetric, steeply dipping northwestern flank and gently southeastern flank. It consists of three lithotectonic units: gneissic migmatite unit, Paleo‐ to Meso‐Proterozoic micaschist‐slate Neoproterozoic Mesozoic sedimentary cover. Three deformation events related extensional tectonics are distinguished in study area: D1 ductile...
Middle Triassic orogens are widespread around and inside the South China Block (SCB). The southern peripheral belts that develop from northwest to southeast, namely Jinshajiang, Ailaoshan, NW Vietnam, NE Yunkai Hainan exhibit striking similarities, with Permian–Early magmatic arc, ophiolitic mélange, northeast- north-directed synmetamorphic ductile nappes, fold-and-thrust belt. These collisional result oceanic, then continental subduction of SCB below Indochina. Eastward Island, a suture is...
Abstract In the Cretaceous, subduction of Izanagi/Paleo‐Pacific plates beneath South China Block (SCB) created a wide back‐arc domain characterized by numerous extensional basins coeval with voluminous magmatism. The SCB witnessed whole evolution records widespread structures to accommodate lithospheric stretching. interior SCB, Yuechengling (YCL) Massif preserves large, low‐angle detachment fault, Ziyuan Detachment (ZYD) at western margin, and high‐angle ductile normal Tianhu Fault (THF),...
In eastern China, the Sulu area is recognized as extension of Qinling‐Dabie Belt, which famous for its ultrahigh‐pressure (UHP) metamorphism. Although numerous petrologic and geochemical works are available, structural data still rare. This paper provides first extensive study bulk geometry kinematic analysis Shandong Peninsula. The divided into three tectonic areas by Cretaceous faults, namely, a southern UHP belt or area, northern migmatite an eclogite Weihai area. Conversely to deeply...
In south China the Lushan massif forms a topographic high of South Block Qinling‐Dabie belt. The consists two main lithotectonic units separated by major tectonic contact: Neoproterozoic (upper Sinian)‐Paleozoic unit comprising primarily unmetamorphosed sandstones overlies Paleoproterozoic mainly composed low‐pressure, high‐temperature gneisses and micaschists. Both are cut Cretaceous granitic intrusions. Three primary tectono‐metamorphic magmatic events recognized. eastern part is NNE‐SSW...
Abstract The cause of magmatic tempo in an active plate margin remains controversial, partly due to lack structural analysis. During 130–105 Ma, the magmatism South China Block (SCB) was significantly reduced (lull) and restricted around Changle‐Nan'ao Belt (CNB) while highly (flare‐up) North China. For unveiling tectonic role on magmatism, a multidisciplinary study including field microscopic observations, magnetic fabric measurement (AMS), zircon/monazite dating conducted plutons with...