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 …

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 …

华南地区中生代动力体制经历了从特提斯构造域向滨太**洋构造域的转换,
但对这种动力体制转换发生的时间和产生的地质效应则存在不同的认识. 通过分析华南印支 …

华南地区中生代构造动力体制经历了从特提斯构造域向滨太**洋构造域的转换,
由此产生了**烈的陆内造山作用和岩浆活动, 形成了复杂构造组合的晚中生代陆内造山带和 …

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 …

华南地区早中生代经历了**烈的构造变形和岩浆活动, 构造动力体制发生了重大的转换.
这个时期大地构造过程及其发生的构造动力学背景一直是地学界争议的焦点问题之一 …

A mineral that forms under conditions as variable as diagenesis to deep subduction, melt
crystallization to low temperature alteration, and that retains information on time …

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 …

总结出郯庐断裂带中生代运动学演化的过程与历史, 概括为“两大运动时期, 五个发展阶段”.
第一运动时期对应于三叠纪—早侏罗世早期的“印支运动”, 以扬子陆块与华北地块之间的拼合和 …