A5038718201- Geological and Geophysical Studies
- earthquake and tectonic studies
- Geological formations and processes
- Geological Studies and Exploration
- Earthquake Detection and Analysis
- High-pressure geophysics and materials
- Seismology and Earthquake Studies
- Geological and Geochemical Analysis
- Hydraulic Fracturing and Reservoir Analysis
- Hydrocarbon exploration and reservoir analysis
- Drilling and Well Engineering
- Methane Hydrates and Related Phenomena
- Geotechnical and Geomechanical Engineering
China University of Geosciences
2018-2024
Centre National de la Recherche Scientifique
2021-2022
Institut Terre & Environnement de Strasbourg
2022
Université de Strasbourg
2021-2022
Ecole Nationale du Génie de l'Eau et de l'Environnement de Strasbourg (ENGEES)
2021-2022
China Earthquake Administration
2013-2014
Abstract One fundamental lesson from the last decade's research into rifted margins is that stratigraphic horizons cannot be simply correlated proximal distal domain, which makes interpretation of poorly calibrated and largely inaccessible difficult. In this contribution, we propose a new tectono‐stratigraphic model to help break through proximal/distal frontier. After reviewing scientific advances on achieved during century, describe primary spatio‐temporal evolution active deformation...
Abstract Based on a high‐resolution seismic reflection data set, we describe and map rift domains at the tip of V‐shaped NW‐South China Sea (NW‐SCS) Basin. We compare our domain with refraction, magnetic gravity field data, previously mapped Continent‐Ocean Boundaries (COB). also define syn‐breakup sedimentary magmatic sequences across sediment‐rich NW‐SCS, which enables us to reconstruct tectono‐stratigraphic evolution area. This work discuss 3D architecture nature crust investigate how...
Abstract The formation of a new plate boundary and creation the first oceanic crust, two most important processes tectonics, still remains little understood. While older studies used to assumed sharp ocean-continent between continent ocean, recent suggest progressive oceancontinent transition (OCT) unequivocal continental crusts. In latter view, breakup is not instantaneous but lasting phase, which raises questions about nature OCT basement operating lithospheric breakup. Based on detailed...
This study presents evidence of the evolution proto-oceanic crust at South China Sea through magmatic, tectonic, and stratigraphic analysis. The was obtained by interpreting seismic profiles across V-shaped tip Southwest Sub-basin(SWSB) Sea (SCS). SCS is largest marginal sea Southeast Asia located intersection Tethys Pacific subduction zones. SWSB end propagation SCS Ridge, where lithosphere in a critical state breakup. region formed an Oceanic-Continental Transition(OCT)...
Conventional and general reconstruction is the main way for carbonating horizontal wells, communication between acid fracturing reservoir limited. The well section long, filtration loss huge, acid-rock reaction speed fast, serious. Therefore, it necessary to study staged acidizing technology wells start with development of tools form a series in deep carbonate rocks.
<p>Rifted margins are either classified as volcanic vs. non-volcanic or magma-rich magma-poor. While such classifications essentially based on the magmatic budget observed at rifted margins, they do not take into account relative timing of activity with respect to tectonic activity, i.e. when and where first magma forms. High-quality reflection refraction seismic surveys combined drill hole data field observations show that a binary classification is unable satisfactorily...
摘要: 基于跨南海西南次海盆V型尖端区共轭被动大陆边缘的1 000 km长的深反射地震剖面的解释和分析，深入研究南海临界破裂区地壳结构、盆地构造地层格架和岩浆作用特征，阐明地壳岩石圈的伸展破裂过程.结果表明，在南海西南次海盆共轭陆缘可以识别出3条一级界面，即海底、基底（Tg/Tb）和Moho面，根据这些界面可将共轭边缘划分为箱型域、细颈域、楔型域和薄箱型域等多个地壳基底结构构造特征显著不同的构造单元；在西南次海盆V型尖端陆缘盆地充填序列中识别出岩石圈裂解分离的响应界面，即裂后不整合界面T50/Tm，该界面与基底面Tg/Tb限定了陆缘盆地的同裂陷沉积充填序列，其内发育了T70、T60两条重要的幕式构造响应界面，控制了早期高角度正断层控制的断陷盆地系（Tg-T70）、中期拆离断层控制的拆离盆地系（T70-T60）和晚期断坳转换作用控制的坳陷盆地（T60-T50）；西南次海盆V型尖端薄箱型域属于原洋洋壳域，为岩浆型地壳，代表了岩石圈临近裂解分离、但支撑稳定态海底扩张的地幔对流系统还未完全建立起来之前的“临界破裂”状态，发育于23.5~15.5...
The Editors of Journal Food Chemistry and Nanotechnology ( JFCN
<p>Our study focuses on the Zhongjianna (ZJN) (Phu Kham) Basin, located at western termination of South China Sea (SCS) and separated from Indochina continent by N-S striking East Vietnam Boundary Fault Zone, which is a large scale strike-slip fault system. The sedimentary infill history ZJN basin records complete evolution interaction Indochina-SCS system allows tectonic kinematic to be understood.. discovery hyper-extended continental crust mantle exhumation in this leads...