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 …

As a major component of continental crust, granites have been served as the most important
subject in geology. Based on advancements obtained during past decades, this paper …

在全球Rodinia 超大陆的构造框架中, 华夏地块占有突出的地位. 然而, 华夏地块在国内一直存在
不同认识, 其核心一是年龄, 二是范围. 根据出露在研究区的中-高级变质岩, 韧滑流变形迹和近年 …

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 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 …

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 …

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 …