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 …

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 …

Rifted margins are the result of the successful process of thinning and breakup of the
continental lithosphere leading to the formation of new oceanic lithosphere. Observations on …

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 …

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 …

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 …

Three‐dimensional seismic and well data from the deepwater Xisha Trough are used to
investigate the rift structure and sediment infill of a region formed adjacently to the initial …

Rifted margins result from continental lithosphere extension, breakup, and transition to
seafloor spreading by modes typically described by end‐member conceptual models …

Abstract A three‐dimensional (3D) P‐wave seismic velocity (Vp) model of the crust in the
northern South China Sea margin drilled by IODP Expeditions 367/368/368X has been …