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Ze Liu

Researcher at Ocean University of China

Publications -  8
Citations -  224

Ze Liu is an academic researcher from Ocean University of China. The author has contributed to research in topics: Continental margin & Subduction. The author has an hindex of 5, co-authored 8 publications receiving 93 citations.

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Eastward tectonic migration and transition of the Jurassic-Cretaceous Andean-type continental margin along Southeast China

TL;DR: Using multiple disciplinary data comprising seismic profiles, field observations and numerical paleo-topographies, the authors synthetically focused on the Jurassic-Cretaceous evolution and geodynamics of the Andean-type Southeast China continental margin.
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Accretion of oceanic plateaus at continental margins: Numerical modeling

TL;DR: In this article, the authors investigate the dynamics of oceanic plateau accretion at active continental margins using a thermo-mechanical numerical model and find that a thinned continental margin of the overriding plate, weak layers in the oceanic lithosphere, and a young oceanic plateau are three major factors for the accretion.
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Structural and kinematic analysis of Cenozoic rift basins in South China Sea: A synthesis

TL;DR: In this article, the authors performed a comprehensive analysis of seismic profiles and fault architecture data with a view to understand the Cenozoic tectonic evolution of the northern margin of the South China Sea (SCS).
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When plateau meets subduction zone: A review of numerical models

TL;DR: In this paper, the authors review the current state of this field and discuss types of oceanic plateaus subduction by combining and comparing natural observations and numerical models, and identify three modes of Oceanic Plateau subduction in both nature and models.
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Deep-shallow coupling response of the Cenozoic Bohai Bay Basin to plate interactions around the Eurasian Plate

TL;DR: In this article, the authors compared both deep and shallow responses and processes of the Bohai Bay Basin in the Cenozoic and then matched reasonable geodynamic mechanisms for each of them.