The North China Craton (NCC) was originally formed by the amalgamation of the eastern
and western blocks along an orogenic belt at∼ 1.9 Ga. After cratonization, the NCC was …

Abstract The Mesozoic Western Pacific subduction system significantly impacted the North
China and South China blocks along the East Asian continental margin and influenced the …

Abstract The East Asian continent records a complex geologic and tectonic history that
involved the amalgamation of several small-to medium-sized blocks from Laurasia or …

Eastern China provides a precious opportunity to explore how subduction drives evolution of
the overlying continental lithosphere and to understand the fate of subducted plates. In this …

The Asian continent consists of many continental blocks that assembled during the
Phanerozoic, accompanied by widespread granitoids. By compiling a series of digital maps …

The Yanshan movement/orogeny has been proposed for 90 years, which is of special
significance in the history of geological research in China. This study conducted a review by …

Abstract The North China Craton (NCC) experienced strong destruction (ie, decratonization)
during the Mesozoic, which triggered intensive magmatism, tectonism and thermal events …

Cretaceous rift basin evolution was an important part of the tectonic history of northeast Asia
in the late Mesozoic. Three types of rift basins are identified—active, passive and wide rift …

The study of large-scale and long-term sedimentary hiatus and exhumation in vast intraplate
basins is of great significance for unravelling their tectonic development, morphodynamics …

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