Variations of crustal thickness and average Vp/Vs ratio beneath the Shanxi Rift, North China, from receiver functions

Abstract The Shanxi Rift located in the central part of the North China Craton (NCC) as a boundary between the Ordos block and the Huabei basin. The Shanxi graben system is a Cenozoic rift and originated from back-arc spreading related to westward subduction of the western Pacific and far field effe...

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Bibliographic Details
Main Authors: Yifang Chen, Jiuhui Chen, ShunCheng Li, Zhanyang Yu, Xuzhou Liu, Xuzhang Shen
Format: Article
Language:English
Published: SpringerOpen 2021-10-01
Series:Earth, Planets and Space
Subjects:
Online Access:https://doi.org/10.1186/s40623-021-01528-8