There developed four groups of fault with varied orientations in the Central Tarim Lower
Uplift, the middle segment of the Central Rise of Tarim Basin. The NW-striking Central Tarim …

The Tumxuk fault zone in the western Tarim Basin is a boundary between the Bachu Fault-
Uplift, a sub-order unit of the Central Rise whose predecessor was a Jinningian collisional …

Based on systematic interpretation of seismic profiles and a comparative study to central
area of the Tarim Basin, the active modes and mechanisms of the Paleozoic faultings in …

The Manshen-1 fault belt trending in NEE-SWW direction and located in the central Tarim
Basin was revealed during our careful 3D seismic interpretation. It is consisted of numerous …

On the basis of careful seismic interpretation, the Mid-Paleozoic extensional structures were
discovered for the first time in the East Tarim Basin. They are normal faults and their …

There is a NE-SW extend saddle-shaped lower ridge between Awati and Manjiaer sags,
central Tarim Basin. It is proposed as the separate boundary between these two sags. The …

This article aims to analyze the main controlling factors of development, distribution and
evolution of the fault systems in the Tarim Basin. Based on the seismic profile interpretation …

The South Tianshan on the southern margin of the Central Asian Orogenic Belt (CAOB) is a
collisional orogenic belt between the Tarim continent and Ili‐Central Tianshan volcanic arc …

Late Cenozoic normal faults are developed around Awati Sag, NW Tarim Basin. In which,
the Quaternary normal fault activities is the first discovery of structural study in Tarim Basin …

Based on three-dimensional seismic interpretation, structural and sedimentary feature
analysis, and examination of fluid properties and production dynamics, the regularity and …