Major factors controlling fracture development in the Middle Permian Lucaogou Formation tight oil reservoir, Junggar Basin, NW China

Tectonic history of the Irtysh shear zone (NE Kazakhstan): new constraints from zircon U/Pb dating, apatite fission track dating and palaeostress analysis.

Multiple-stage migration and accumulation of Permian lacustrine mixed oils in the central Junggar Basin (NW China)

The Wulungu Depression is the northernmost first-order tectonic unit in the Junggar Basin. It can be divided into three sub-units: the Hongyan step-fault zone, the Suosuoquan sag and the Wulungu south slope. The Cenozoic strata in the basin are intact and Mesozoic–Cenozoic deformation can be observed in the Wulungu step-fault zone, so this is an ideal place to study the Mesozoic–Cenozoic deformation. By integration of fault-related folding theories, regional geology and drilling data, the strata of the Cretaceous–Paleogene systems are divided into small layers which are selected as the subjects of this research. The combination of the developing unconformity with existing growth strata makes it conceivable that faults on the step-fault zone have experienced different degrees of reactivation of movement since the Cretaceous. Evolutionary analyses of the small layers using 2D-Move software showed certain differences in the reactivation of different segments of the Wulungu Depression such as the timing of reactivation of thrusting, for which the reactivity time of the eastern segment was late compared with those of the western and middle segments. In addition the resurrection strength was similarly slightly different, with the shortening rate being higher in the western segment than in the other segments. Moreover, the thrust fault mechanism is basement-involved combined with triangle shear fold, for which a forward evolution model was proposed.

Large-scale thrusting at the northern Junggar Basin since Cretaceous and its implications for the rejuvenation of the Central Asian Orogenic Belt

Constraints of tectonic uplift and denudation on sandstone-type uranium mineralization in Meso-Cenozoic basins in northern China: A review

Metal source and ore precipitation mechanism of the Ashawayi orogenic gold deposit, southwestern Tianshan Orogen, western China: Constraints from textures and trace elements in pyrite

Early Paleozoic Tectonic Evolution of the Chinese Southwest Tianshan Orogen: Implications from Detrital Zircon U‐Pb Geochronology of the Biedieli Sedimentary Rocks, Northern Wushi Area, NW China

The arc-shape Pamir tectonic belt is located on the northwestern margin of the Tibetian plateau. At present, there are many different understandings on the history of the Pamir Plateau uplift, mainly on the time of uplift, which seriously affects the understanding of the global paleo-environmental changes since the Cenozoic. The method of reconstructing paleoelevation based on lava vesicles has improved in recent years, providing the means for establishing reliable constraints on the uplift time of the Pamir plateau. We studied Cenozoic vesicular basalt from the Tuoyun Basin in the northeastern margin of the Pamir tectonic belt. We used a lava-vesicle paleoaltimeter that measured vesicle volume at the tops and bottoms of two basalt layers, allowing the elevation of the Tuoyun Basin during the Eocene to be reconstructed according to the relationship between atmospheric pressure and altitude. Results show that the Tuoyun Basin had reached the elevation of > 2000 m at ca. 48 Ma, indicating that the influence of the Pamir tectonic belt on the Tianshan Mountains began during the Eocene. This new finding offers our contribution to better understand the impact the uplift of the Tibetian plateau on the Tianshan region and the environmental changes in central Asia during the Cenozoic. 

Eocene paleoelevation of the Tuoyun Basin, northeastern Pamirs: Evidence from a lava-vesicle-based paleoaltimeter

Mesozoic differential uplift-exhumation processes in the western Tian Shan, Uzbekistan: Constraints from apatite/zircon fission track and (U Th)/He thermochronology

Exhumation Degree of Intrusions in the Kangguer–Huangshan Area and Its Constraint on Ore‐Preservation in the Jueluotage Tectonic Belt, Eastern Tianshan

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