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 …

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 Qinling Orogenic Belt (QOB) is located between the North China and South
China Blocks, and has been considered to have formed by the collision between these …

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 …

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 …

The continental crust of China is a mosaic of cratonic blocks and orogenic belts, containing
small cratons and terranes with various tectonic settings. They have diverse origins and …

This contribution reviews the tectonic structure and evolution of the Qinling orogenic belt,
which extends east–west nearly 2500 km across Central China and is a giant orogenic belt …

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 …

The Qinling Orogen is one of the main orogenic belts in Asia and is characterized by multi-
stage orogenic processes and the development of voluminous magmatic intrusions. The …

Abstract The Qinling Orogenic belt has been well documented that it was formed by multiple
steps of convergence and subsequent collision between the North China and South China …