A5013107746- Geological and Geochemical Analysis
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- earthquake and tectonic studies
- Geochemistry and Elemental Analysis
- Geochemistry and Geochronology of Asian Mineral Deposits
- Paleontology and Stratigraphy of Fossils
- Geomagnetism and Paleomagnetism Studies
- Geology and Paleoclimatology Research
- Hydrocarbon exploration and reservoir analysis
- Geological Studies and Exploration
- Geological and Geophysical Studies
- Paleontology and Evolutionary Biology
- Isotope Analysis in Ecology
Chengdu University of Technology
2021-2025
Nanjing University
2014-2020
University of Arizona
2019
University of New Caledonia
2017-2019
Research Article| August 29, 2017 Accretionary tectonics of back-arc oceanic basins in the South Tianshan: Insights from structural, geochronological, and geochemical studies Wuwamen ophiolite mélange Bo Wang; Wang † 1State Key Laboratory for Mineral Deposits Research, School Earth Sciences Engineering, Nanjing University, 210093 Nanjing, China †bwang@nju.edu.cn Search other works by this author on: GSW Google Scholar Yazhong Zhai; Zhai Paul Kapp; Kapp 2Department Geosciences, University...
Abstract The southeastern (SE) Tibetan Plateau (Yunnan) is characterized by low‐relief uplands that were deeply incised large rivers. thermal history of basement rocks in this region remains poorly investigated, while data needed to elucidate the complex relationship between tectonics and climate shaping surface. To better understand its thermo‐tectonic evolution, we carried out apatite fission track thermochronology on 31 samples collected from a area covers different tectonic units,...
The Tibetan Plateau geographically contains internal and external drainage areas based on the distributions of river flows catchments.The display similar highelevations, while their topographic reliefs are not comparable; former shows a large low-relief surface, whereas latter is characterized by relatively high relief.The eastern Lhasa terrane key tectonic component Plateau.It topography relief, but thermal history its basement remains poorly constrained.In this study we report new apatite...
The Tibetan Plateau is currently the widest and highest elevation orogenic plateau on Earth. It formed as a response to Cenozoic still ongoing collision between Indian Eurasian plates. Xigaze fore-arc basin located along suture zone of both plates, i.e. Indus Yarlung in southern Tibet. This area preserves important information related late tectonic topographic evolution plateau. In this study, apatite fission track (AFT) thermochronology was carried out twelve sandstone samples from middle...
Abstract The coupling of magnetic fabrics and remanences is critical in interpreting paleomagnetic data. To estimate whether primary imply remanences, to assess the practicability metamorphic rocks study, we carried out petrographic, geochronological, rock investigations, analyses anisotropy susceptibility paleomagnetism on migmatites Central Tianshan, NW China. Petrological observations indicate no significant dynamic recrystallization post migmatization. In‐situ monazite U‐Pb dating...
Bogda Shan is a mountain belt located at the eastern extremity of Chinese Tianshan and records complex debated exhumation history. Previous studies have reported young Cenozoic thermal history for Shan, which in conflict with observation preserved Mesozoic erosion surfaces area. This study re-evaluates Meso-Cenozoic thermo-tectonic evolution using apatite fission track (AFT) thermochronology. Palaeozoic basement (meta-sandstone) samples collected from northern southwestern flanks ranges...
The large Gangdese metallogenic belt, located in the southern part of Tibetan Plateau, hosts a variety magmatic-hydrothermal ore deposits. Previous works area primarily concerned genesis, while exhumation history these deposit has received less attention. In this contribution we explore multi-stage thermo-tectonic evolution Longmala and Mengya'a Pb-Zn deposits, two deposits central Lhasa sub-terrane. more detail, thermal granitoids deformed Paleozoic sediments inside on periphery districts...
Abstract The Tibetan Plateau is currently the widest and highest elevation orogenic plateau on Earth. It formed as a response to Cenozoic still ongoing collision between Indian Eurasian plates. Xigaze fore-arc basin distributed along Indus–Yarlung suture zone in southern Tibet preserves important information related late tectonic topographic evolution of plateau. In this study, apatite fission track (AFT) thermochronology was carried out twelve sandstone samples from middle segment...
The Altai orogenic belt is a main constituent of the Central Asian Orogenic Belt, and serves as crucial site for studying strain propagation from Meso-Cenozoic plate margins to Eurasian interior. ranges Mountains have undergone multiple reactivation events during Mesozoic Cenozoic, but full extent these not yet fully understood. To constrain thermo-tectonic history southern Northwest China, apatite fission-track (AFT) (U-Th)/He (AHe) thermochronological methods were used study 29...
The Narusongduo Pb-Zn deposit is located at the northern boundary of Luobadui-Milashan fault zone (LMF) in central Tibet and spatially associated with Linzizong volcanic succession (LVS). Our study indicates that regional structural setting was formed by two-stage tectonic events. first stage, spanning from late Mesozoic to early Paleocene, characterized significant N-S crustal shortening Cordilleran-type orogeny along Gangdese arc. region's Paleozoic-Mesozoic metasedimentary rocks were...