Approximately 1.78 Ga mafic dykes in the Lüliang Complex, North China Craton: Zircon ages and Lu-Hf isotopes, geochemistry, and implications-Reference-Cited by-同舟云学术

Approximately 1.78 Ga mafic dykes in the Lüliang Complex, North China Craton: Zircon ages and Lu-Hf isotopes, geochemistry, and implications

Published:2014-08 Issue:8 Volume:15 Page:3123-3144
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Wang Xi¹,Zhu Wenbin¹,Luo Meng²,Ren Xingmin¹,Cui Xiang¹

Affiliation:

1. State Key Laboratory for Mineral Deposits Research, Department of Earth Sciences; Nanjing University; Nanjing People's Republic of China

2. Department of Civil Engineering; Wentian College, Hohai University; Ma'anshan People's Republic of China

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

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4. Middle Paleoproterozoic crustal extensional regime in the North China Craton: New evidence from SHRIMP zircon U-Pb dating and whole-rock geochemistry of meta-gabbro in the Anshan-Gongchangling area [in Chinese];Dong;Acta Petrol. Sin.,2012

5. The 2.2-2.1Ga magmatic event and its tectonic implication in the Lüliang Mountains, North China Craton [in Chinese];Du;Acta Petrol. Sin.,2012

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