A5058908812- earthquake and tectonic studies
- Geological and Geochemical Analysis
- Geological and Geophysical Studies
- Geology and Paleoclimatology Research
- High-pressure geophysics and materials
- Hydrocarbon exploration and reservoir analysis
- Geochemistry and Geologic Mapping
- Seismology and Earthquake Studies
- Geomagnetism and Paleomagnetism Studies
- Geological formations and processes
- Methane Hydrates and Related Phenomena
- Landslides and related hazards
- Geochemistry and Geochronology of Asian Mineral Deposits
- Geological Studies and Exploration
- Geoscience and Mining Technology
- Paleontology and Stratigraphy of Fossils
- Earthquake Detection and Analysis
- Remote Sensing and Land Use
- Seismic Waves and Analysis
- Seismic Imaging and Inversion Techniques
- Marine and environmental studies
- Rock Mechanics and Modeling
- Nanoplatforms for cancer theranostics
- Geotechnical and Geomechanical Engineering
- Advanced Decision-Making Techniques
Chinese Academy of Geological Sciences
2015-2025
Ministry of Natural Resources
2017-2025
Dalian University of Technology
2025
Dalian University
2025
Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)
2021-2024
Second Artillery General Hospital of Chinese People's Liberation Army
2024
Huazhong Agricultural University
2024
Yingkou Institute of Technology
2024
Czech Academy of Sciences, Institute of Geology
2020-2023
Heriot-Watt University
2018-2023
Abstract The Xianshuihe (XSH) fault in eastern Tibet is one of the most active faults China, with next large earthquake likely to occur along its SE part, where splits into three parallel branches: Yalahe, Selaha and Zheduotang (ZDT). Precisely quantifying their slip rates at various timescales essential evaluate regional hazard. Here, we expand our previous work on nearby ZDT Moxi (MX) faults, add observations Yalahe newly discovered Mugecuo South zone. Using tectonic‐geomorphology...
Phototherapy has remarkable advantages in cancer treatment, owing to its high efficiency and minimal invasiveness. Indocyanine green (ICG) plays an important role photo-mediated therapy. However, it several disadvantages such as poor stability aqueous solutions, easy aggregation of molecules, short plasma half-life. This study aimed develop efficient nanoplatform enhance the effects We developed a novel bio-nanoplatform by integrating edible ginger-derived exosome-like nanoparticles (GDNPs)...
Research Article| September 12, 2017 Temporally constant slip rate along the Ganzi fault, NW Xianshuihe fault system, eastern Tibet Marie-Luce Chevalier; Chevalier † 1Key Laboratory of Continental Dynamics, Institute Geology, Chinese Academy Geological Sciences, 26 Baiwanzhuang Road, Beijing 100037, People's Republic China †mlchevalier@hotmail.com; herve.leloup@univ-lyon1.fr; anne.replumaz@ujf-grenoble.fr; jiawei-pan@foxmail.com; marianne.metois@univ-lyon1.fr; lihaibing06@163.com. Search for...
Abstract Transient sediment storage and mixing of deposits various ages during transport across alluvial piedmonts alter the clastic sedimentary record. We quantify buffering cycles aggradation–incision in north piedmont Eastern Tian Shan. complement existing chronologic data with 20 new luminescence one cosmogenic radionuclide age terrace abandonment aggradation. Over last 0.5 Myr, deeply incised aggraded many times per 100 kyr. Aggradation is driven by an increased flux glacial accumulated...
Abstract The presence of ~NS‐trending rifts within the Tibetan Plateau attests that it is undergoing ~EW extension. In southern Tibet, total extension rate, distributed across seven main over a distance ~1,000 km, has been inferred to amount about half shortening rate Himalayas. Quantifying late Quaternary rates largest rift (Yadong‐Gulu [YGR]) important understand deformation and discuss high plateau evolution during later stages continental collision. We performed 10 Be surface‐exposure...
[1] The exact location of the northern Karakorum fault (KF) in western Tibet is unclear and its current activity debated. Here, we investigate possible extension KF, Muji fault, located Chinese Pamir, which belongs to Kongur Shan extensional system, provide first quantitative estimate Holocene slip-rate. cuts offsets a series 6 fluvial terraces, yielding minimum slip-rate 4.5 ± 0.2 mm/yr, by matching largest terrace riser offset with upper surface age (10Be, n = 24). Field evidences...
Field investigations reveal that the 2014 M w 6.9 Yutian earthquake on left‐lateral strike‐slip Altyn Tagh fault (ATF) system, Tibetan Plateau, produced an ∼25‐km‐long surface rupture zone contains conjugate Riedel shear faults. The coseismic ruptures occurred mainly along two parallel east‐northeast‐trending active Rupture also in a conjugate, west‐northwest‐trending right‐lateral fault. are concentrated of <500‐m wide and ∼25‐km long, characterized by structures including distinct faults...
Determining the provenance of sedimentary basin fill in northern Qaidam Basin is a key step toward understanding system dynamics and mountain-building processes surrounding orogenic belts Tibet. The exceptionally thick (average 6–8 km) Cenozoic fluvio-lacustrine deposits were once thought to have been eroded from nearby margin southern Qilian Shan reflect prolonged thrust-related exhumation these belts. However, several recent studies, based mainly on paleocurrent detrital zircon U-Pb age...
Abstract Sedimentary rocks in northern Tibet record uplift of the Tibetan Plateau and its potential connection with evolution central Asian aridity, therefore offering a typical example tectonic-climate linkage. The coarse-grained conglomeratic sandy red beds Lulehe Formation (Fm.) Qaidam Basin (QB), Tibet, have long been held as synorogenic sediment accumulation. There is, however, heated debate on source area (the Qilian Shan, east Kunlun or Qimen Tagh) initiation age (ca. 52, 25.5, ca. 21...
Abstract The Tibetan Plateau stands as a prominent topographic feature at the Earth's surface, characterized by intense seismic activity, in particular along its bounding mountain ranges. To northwest, Western Kunlun Range has received increasing attention since 2015 Pishan earthquake but kinematics of deformation remain to be properly documented. Here, we analyze terrace record active Karakash River, where it crosses Hotan anticline. We date terraces using situ produced cosmogenic isotopes,...
Abstract The widespread appearance of intermontane basins in the northern Tibetan Plateau herald outward expansion tectonic deformation into sedimentary basins. When and how have been deformed segmented, however, remain still unexplored. Qaidam basin, biggest basin Tibet, archives up to 20 km‐thick succession ranging age from Paleozoic Cenozoic. To tackle this issue, here we present a relatively large apatite fission track data set, coupled with detailed structural observations, for...