The Cretaceous tectonic evolution of South China is characterized by widespread
extensional basin and dome generation, voluminous magma intrusion/eruption and …

The basic tectonic framework of continental East Asia was produced by a series of nearly
contemporaneous orogenic events in the late Middle Jurassic to Early Cretaceous …

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 Youjiang Basin in the western part of the South China Block (SCB), preserves
the records of the tectonic history from Tethyan, through Paleo-Pacific to Tibetan domains …

In the Cretaceous, the subduction of the Izanagi/Paleo‐Pacific plates beneath the South
China Block (SCB) created a wide back‐arc domain characterized by numerous extensional …

South China hosts the most abundant and largest tungsten (W) deposits in the world, being
a famous W metallogenic region. Located at the eastern part of the South China Block …

Understanding the Mesozoic intraplate structural response of South China inboard of the
Paleo-Pacific-South China convergent margin is a key issue in unravelling the continental …

Located in the southeastern margin of the Yangtze Block and generally interpreted as the
Neoproterozoic collisional product of the Yangtze with the Cathaysia Blocks of South China …

Multi-plate convergence around a nuclear block and the geodynamic transition occurred
generally after the onset of plate tectonics. Late Triassic to Middle Jurassic geodynamics of …

Abstract The central Jiangnan Orogen, genetically formed by the Proterozoic Yangtze‐
Cathaysia collision, presents as a composite structural feature in the Phanerozoic with …