Angular Unconformity of the Late Quaternary Strata in the Hetao Basin, North of the Ordos Block (West China): Timing and Its Tectonic Implications

Following the uplift of the Tibet Plateau and the continuous subduction of the Pacific Plate, graben faulting began to appear around the Ordos Block in the Cenozoic. The Hetao Basin is a Cenozoic rift basin between the Ordos Block and the Yinshan Mountains, and Late Quaternary sedimentary strata, wh...

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Bibliographic Details
Main Authors: Luanxi Bai, Xiwei Xu, Hao Luo, Kang Li, Xibin Tan, Junxiang Zhao
Format: Article
Language:English
Published: Frontiers Media S.A. 2021-03-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2021.646789/full