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 …

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

华南至少经历了4 期区域规模的大陆动力学过程, 除新元古代和晚中生代具有活动陆缘背景外,
均在板块内部发生并完成. 华夏块体是一个以新元古代岩石为主体构成的前南华纪基底 …

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 …

Establishing how tectonic plates have moved since deep time is essential for understanding
how Earth's geodynamic system has evolved and operates, thus answering longstanding …

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 …

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 …

We present a review of major gold mineralization events in China and a summary of
metallogenic provinces, deposit types, metallogenic epochs and tectonic settings. Over 200 …

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 …

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