Interactions between tectonic, magmatic, sedimentary and hydrothermal processes during
rifting and break-up of continental lithosphere lead to a variety of rifted margin types. As …

Southeast Asia is located in an important regional geodynamic intersection zone
surrounded by inward subduction systems on three sides, consisting the largest and most …

The interaction between magmatic and extensional processes related to the formation of
rifted margins has been and still is highly debated. The interpretation of magmatic additions …

Abstract Ocean-Continent Transition (OCT) located between the edge of the continental and
unequivocal oceanic crusts is an ideal laboratory to understand one of the most fundamental …

边缘海如何形成是地球科学的基本问题. 本研究通过对南海区域深反射地震数据及钻井数据的
综合解释, 聚焦地壳深部结构和三维全变形机制, 在南海陆缘张裂-海盆扩张的构造动力学研究中 …

Rheological differences may lead to discrepant thinning order of the crust and lithospheric
mantle when the continent is passively stretched. The crust breaks up earlier than the …

南海北部陆缘发育独特的远端带结构, 以“裂谷宽, 基底厚和地貌起伏” 为主要特点,
显著有别于经典贫岩浆型和富岩浆型张裂陆缘. 为了解释陆缘结构的成因, 综合已有研究进展和 …

Abstract The northern South China Sea (SCS) margin developed on a thinning crust
comprising basement-involved structures inherited from the post-orogenic extension of the …

We present a new extensional tectonic model for the Cenozoic history of SE Asia and the
opening of the South China Sea (SCS), proposing a feedback mechanism by which …

Continent-ocean transition (COT) is a key area for studying the lithospheric replacement
from the thinned continental to oceanic crust. The extent and nature of the COT in the mid …