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 …

Subduction and closure of the Proto-Tethys and Palaeo-Tethys oceans were important
events in the assembly of Eurasia, and created the Central China Orogenic Belt (CCOB) …

As the chronicle of plate motions through time, paleogeography is fundamental to our
understanding of plate tectonics and its role in shaping the geology of the present-day. To …

The Qilian Orogen at the northern margin of the Tibetan Plateau is a type suture zone that
recorded a complete history from continental breakup to ocean basin evolution, and to the …

摘要分布在青藏高原北缘的阿尔金 祁连 柴北缘早古生代造山系被认为是原特提斯构造域最
北部的构造拼合体. 与其北侧具有长期增生历史的中亚造山系相比, 特提斯造山拼合体被认为是 …

祁连山地区的新元古代中-晚期至早古生代火山作用显示系统地时, 空变化,
其乃是祁连山构造演化的火山响应. 随着祁连山构造演化从Rodinia 超大陆裂谷化-裂解 …

The Qilian Shan, located in the northern Tibetan Plateau of NW China, has an excellent
record of early to middle Paleozoic subduction–accretion that resulted from convergence …

Asia is key to a richer understanding of many important lithospheric processes such as
crustal growth, continental evolution and orogenesis. But to properly decipher the secrets …

Back-arc basins are pivotal sites for the generation and consumption of oceanic lithosphere
in mature intra-oceanic convergent plate margins. However, the processes and mechanisms …

The Chaidanuo granite batholith is a∼ 500 km 2 homogeneous, high-level intrusion in the
North Qilian oceanic suture zone. Three types of enclaves have been recognized, including …