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

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 effects cause...

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Vydané v:	Earth, planets, and space Ročník 73; číslo 1; s. 1 - 14
Hlavní autori:	Chen, Yifang, Chen, Jiuhui, Li, ShunCheng, Yu, Zhanyang, Liu, Xuzhou, Shen, Xuzhang
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Berlin/Heidelberg Springer Berlin Heidelberg 29.10.2021 Springer Springer Nature B.V SpringerOpen
Predmet:	4. Seismology Cenozoic Crust Crustal thickness Earth Earth and Environmental Science Earth Sciences Earthquakes Environmental aspects Geology Geophysics/Geodesy Graben Grabens (Geology) H-κ stacking Heterogeneity Mountains Quaternary Receiver function Seismic activity Shanxi Rift Subduction (geology) Subduction zones (Geology) Tectonics Thickness Vp/Vs ratio China Shanxi China Vp/Vs ratio Crustal thickness Receiver function Shanxi Rift stacking
ISSN:	1880-5981, 1343-8832, 1880-5981
On-line prístup:	Získať plný text
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