The Qilian orogenic system in the northern Tibetan Plateau records the complete tectonic
cycle from opening of Proto-Tethys Ocean, initial subduction, to continental subduction and …

Abstract The Altun–Qilian–Kunlun orogenic system in the northern Tibetan Plateau is
considered as the northernmost orogenic collage of the proto-Tethyan domain. Early …

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 …

Abstract The Altun-Qilian-Kunlun Mountain (AQK), located on the northeastern margin of the
Qinghai-Tibet Plateau, experienced multiple Neoproterozoic magmatic and metamorphic …

Numerous granitic intrusions crop out in the eastern segment of the North Qaidam block
(NQ), NW China. To evaluate their ages, petrogenesis and genetic relationships to other …

Abstract Voluminous Early Paleozoic intrusive rocks occur in the Qilian orogenic belt,
northeastern margin of the Tibetan Plateau. Their petrogenesis can provide insights into the …

The Dunhuang block, which constitutes the northeastern segment of the Tarim Craton, is
located between the Central Asian Orogenic Belt (CAOB) to the north and the Altyn–Qilian …

In the plate tectonics theory, continental subduction is pulled by subduction of dense
oceanic crust. In practice, however, it is not easy to demonstrate that preceding oceanic crust …

The Dunhuang region is located in the east of the Tarim Craton and has long been
considered as part of a Precambrian terrane of the Tarim or North China Craton. Aiming to …

The effects of post-ore metamorphism and deformation on trace element concentrations in
sulfides have recently received increasing attention. In this study, we report comprehensive …