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 The South China Craton consists of the Yangtze and Cathaysia blocks that were
welded together along the Jiangnan Fold Belt in the Neoproterozoic. The Neoproterozoic …

Contrasting models for internal and external locations of South China within the Nuna and
Rodinia supercontinents can be resolved when the current lithotectonic associations of …

Continental China is a mosaic of numerous tectonic blocks, which amalgamated from
Neoarchean to Cenozoic broadly coeval with the cycles of global supercontinents such as …

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 …

Abstract The evolution of South China involved accretion-collision of multiple terranes from
the Proterozoic to the Mesozoic. Zircon U-Pb ages, Hf data, and structural data indicate that …

Oxygen fugacity (fO 2) is a key factor that controls the formation of porphyry Cu deposits.
Porphyry Cu deposits are typically oxidized, but when and how porphyry magmas gain their …

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 …

The correlation between Neoproterozoic tectonics, paleoenvironment and early life are
crucial for understanding the evolution of the Earth's habitability. The Yangtze Block …