U–Pb detrital zircon geochronology and Hf isotopic composition of Permian clastic rocks, Zhen’an basin, South Qinling belt: implications for the Paleozoic tectonic evolution of the Qinling orogenic belt-Reference-Cited by-同舟云学术

U–Pb detrital zircon geochronology and Hf isotopic composition of Permian clastic rocks, Zhen’an basin, South Qinling belt: implications for the Paleozoic tectonic evolution of the Qinling orogenic belt

Published:2018-09-17 Issue:12 Volume:61 Page:1462-1478
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Cheng Cheng¹²,Li Shuangying¹,Xie Xiangyang²^ORCID,Manger Walter L.³,Busbey Arthur B.³

Affiliation:

1. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei, China

2. Department of Geological Sciences, Texas Christian University, Fort Worth, TX, USA

3. Department of Geosciences, University of Arkansas, Fayetteville, AR, USA

Funder

China Geological Survey

China Scholarship Council

National Natural Science Foundation of China

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2018.1517393

Reference92 articles.

1. Geochronology and isotopic character of ultrahigh-pressure metamorphism with implications for collision of the Sino-Korean and Yangtze cratons, central China

2. Slab break-off model for the Triassic syn-collisional granites in the Qinling orogenic belt, Central China: Zircon U-Pb age and Hf isotope constraints

3. The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system

4. Detrital zircon record and tectonic setting

5. 2.6–2.7Ga crustal growth in Yangtze craton, South China

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