Neoproterozoic (750–711 Ma) Tectonics of the South Qinling Belt, Central China: New Insights from Geochemical, Zircon U‐Pb Geochronological, and Sr‐Nd Isotopic Data from the Niushan Complex

Author:

WANG Shuo1,LIU Yunhua1,YANG Benzhao2,TAN Le2,LI Xiaoyan3,DENG Nan4

Affiliation:

1. School of Earth Sciences and Resources Chang'an University Xi'an 710054 China

2. Geological Team No. 1 of Shaanxi Bureau of Geology and Mineral Resources, Ankang Shannxi 725000 China

3. Longshou Mine of Jinchuan Group Co., Ltd, Jinchang Gansu 737100 China

4. Xi'an Mineral Resources Survey Center China Geological Survey Xi'an 710100 China

Publisher

Wiley

Subject

Geology

Reference104 articles.

1. Correction of common lead in U–Pb analyses that do not report 204Pb

2. Neoproterozoic crustal accretion of the northern margin of Yangtze plate: Constrains from geochemical characteristics, LA-ICP-MS zircon U-Pb chronology and Hf isotopic compositions of trondhjemite from Zushidian area, Hannan region;Ao W.H.;Geological Review,2014

3. The Neoproterozoic magmatism in the northern margin of the Yangtze Block: Insights from Neoproterozoic (950–706 Ma) gabbroic-granitoid rocks of the Hannan Complex;Ao W.H.;Gondwana Research,2019

4. The heart of China revisited, I. Proterozoic tectonics of the Qin mountains in the core of supercontinent Rodinia;Bader T.;Tectonics,2013

5. A review of the relationships between granitoid types, their origins and their geodynamic environments

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