Central China orogenic belt and amalgamation of East Asian continents

Y Dong, S Sun, M Santosh, J Zhao, J Sun, D He… - Gondwana …, 2021 - Elsevier
Abstract The Central China Orogenic Belt (CCOB) comprises, from the east to the west, the
Tongbai-Dabie, Qinling, Qilian and Kunlun Orogens, and preserves abundant and important …

Geological reconstructions of the East Asian blocks: From the breakup of Rodinia to the assembly of Pangea

G Zhao, Y Wang, B Huang, Y Dong, S Li, G Zhang… - Earth-Science …, 2018 - Elsevier
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 …

Reconstructing South China in phanerozoic and precambrian supercontinents

PA Cawood, G Zhao, J Yao, W Wang, Y Xu… - Earth-Science …, 2018 - Elsevier
The history of the South China Craton and the constituent Yangtze and Cathaysia blocks are
directly linked to Earth's Phanerozoic and Precambrian record of supercontinent assembly …

Jiangnan orogen, South China: a~ 970–820 Ma Rodinia margin accretionary belt

J Yao, PA Cawood, L Shu, G Zhao - Earth-Science Reviews, 2019 - Elsevier
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 …

Precambrian geology of China

G Zhao, PA Cawood - Precambrian Research, 2012 - Elsevier
China contains three major Precambrian blocks, the North China, South China and Tarim
cratons, separated and sutured by Phanerozoic orogenic belts. The North China Craton …

Jiangnan Orogen in South China: Developing from divergent double subduction

G Zhao - Gondwana Research, 2015 - Elsevier
Abstract The Jiangnan Orogen is considered as a continent–continent collisional belt
resulting from the closure of a Meso-Neoproterozoic ocean separating the southeastern …

Neoproterozoic magmatism in the western and northern margins of the Yangtze Block (South China) controlled by slab subduction and subduction-transform-edge …

JH Zhao, QW Li, H Liu, W Wang - Earth-Science Reviews, 2018 - Elsevier
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 …

Geology and metallogeny of tungsten and tin deposits in China

J Mao, H Ouyang, S Song, M Santosh, S Yuan, Z Zhou… - 2019 - pubs.geoscienceworld.org
Tungsten and Sn deposits in China are widely distributed in the South China block (ie,
Yangtze craton-Cathaysian block), Himalaya, Tibetan, Sanjiang, Kunlun, Qilian, Qinling …

Cross Orogenic Belts in Central China: Implications for the tectonic and paleogeographic evolution of the East Asian continental collage

Y Dong, S Sun, M Santosh, B Hui, J Sun, F Zhang… - Gondwana …, 2022 - Elsevier
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 …

Amalgamation between the Yangtze and Cathaysia Blocks in South China: constraints from SHRIMP U–Pb zircon ages, geochemistry and Nd–Hf isotopes of the …

XH Li, WX Li, ZX Li, CH Lo, J Wang, MF Ye… - Precambrian …, 2009 - Elsevier
South China was formed through the amalgamation of the Yangtze Block with the Cathaysia
Block, but the timing of this amalgamation is controversial, ranging from Mesoproterozoic to …