Abstract The South China Block is situated in the Eastern Asian margin. Since the
Neoproterozoic, its tectonic evolution was constrained by successive consumption-closure …

Pangea is the youngest supercontinent in Earth's history and its main body formed by
assembly of Gondwana and Laurasia about 300–250 Ma ago. As supported by voluminous …

Abstract The Neoproterozoic Jiangnan Orogen in South China records a succession of arc-
trench-basin assemblages culminating in accretion of the bounding Yangtze and Cathaysia …

Abstract Yanshanian (ca. 200–100 Ma) metallogeny of eastern Asia was dominantly
controlled by oblique subduction and rollback of the Izanagi plate, and also, more locally in …

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 …

Lithospheric extension plays a pivotal role in governing the evolution of continents and the
birth of oceanic basins on Earth. Despite this, quantifying wide-mode lithospheric extension …

The Jiaodong gold province in northeastern China is the country's premier gold resource
and globally one of the most important gold provinces. The late Early Cretaceous gold …

The Jiangnan orogenic belt in South China, formed by the collision of the Yangtze and
Cathaysia sub-blocks, represents a key to reconstruct the assembly of the Rodinia …

The central Nanling region in South China was the site of uplift, extensional deformation,
granite magmatism and hydrothermal activity from 180 to 150 Ma. Information on the age …

The northeast Cathaysia area is characterized by an archetypical, transpressional system
with widespread strike‐slip shear zones whose geometries, kinematics, and ages are critical …