A5014780501- earthquake and tectonic studies
- Geological and Geochemical Analysis
- High-pressure geophysics and materials
- Seismic Imaging and Inversion Techniques
- Geological and Geophysical Studies
Laboratoire d’Océanologie et de Géosciences
2024
Zhejiang University
2024
Abstract In the rejuvenated mountain front, preexisting basement structures are often reactivated and interact with subsequent thin‐skinned deformation. How deep affect shallower ones is key to establishing processes mechanisms for foreland fold‐and‐thrust system. We presented an exceptional case study on structural inheritance between Mesozoic strike‐slip faults shallow Cenozoic contractional folds from Northern Tianshan basin, Northwest China, using high‐resolution 2‐D 3‐D seismic data....
In central Asia, the Tianshan mountains have undergone a series of subduction-collision-accretion processes during Paleozoic times that resulted in forming basement structures later reactivated Cenozoic rejuvenation range. northern Tianshan-South Junggar foreland basin, en échelon W-E / WNW-ESE folds constitute large-scale fold-and-thrust belt (FTB). Using recent industrial 2-D and 3-D seismic surveys carried out western area FTB, we analyzed outcropping (Dushanzi Xihu anticlines)...