Detrital zircon analysis of the Mesozoic strata in the northern Ordos Basin: Revealing the source‐to‐sink relationships and tectonic settings-Reference-Cited by-同舟云学术

Detrital zircon analysis of the Mesozoic strata in the northern Ordos Basin: Revealing the source‐to‐sink relationships and tectonic settings

Published:2022-05-25 Issue:8 Volume:57 Page:3251-3266
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Ao Cong¹²,Cheng Yinhang¹²^ORCID,Tang Yuanhe²³,Wang Shaoyi¹²,Teng Xueming¹²,Jin Ruoshi¹²,Zhang Tianfu¹²,Xu Zenglian¹²,Yang Jun¹²,Zhang Chao¹²,Wang Shanbo¹²

Affiliation:

1. Tianjin Center China Geological Survey Tianjin China

2. Laboratory of Uranium Geology China Geological Survey Tianjin China

3. Xi'an Center of Mineral Resources Survey China Geological Survey Xi'an China

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4472

Reference85 articles.

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2. Detrital zircon record and tectonic setting

3. Chang E. Z. Ying X. D. Zhou A. Wang L. B.(1994).Geodynamic evolution of continental margins in Eastern Asia and tectonic setting of East China Sea. In: Coleman R. G. (Ed.) Reconstruction of the Paleo‐Asian Ocean. Proc. 29th Int. Geol. Congress Part B(pp. 133–167). Utrecht The Kingdom of the Netherlands: VSP.

4. Estimation of denudation thickness of Mesozoic stata in the Ordos Basin and its geological significance;Chen R. Y.;Acta Geologica Sinica,2006

5. Provenances of the Mesozoic sediments in the Ordos Basin and implications for collision between the North China Craton (NCC) and the South China Craton (SCC)

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