兴凯地块南部花岗岩年代学、地球化学及Hf同位素特征

敬海鑫; 孙德有; 苟军; 武鹏飞; 王天豪; 郭宏宇; 柳小明; 胡兆初

doi:10.3799/dqkx.2015.082

Volume 40 Issue 6

Jun. 2015

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Article Navigation > Earth Science > 2015 > 40(6): 982-994

Jing Haixin, Sun Deyou, Gou Jun, Wu Pengfei, Wang Tianhao, Guo Hongyu, Liu Xiaoming, Hu Zhaochu, 2015. Chronology, Geochemistry and Hf Isotope of Granite from Southern Xingkai Block. Earth Science, 40(6): 982-994. doi: 10.3799/dqkx.2015.082

Citation:

Jing Haixin, Sun Deyou, Gou Jun, Wu Pengfei, Wang Tianhao, Guo Hongyu, Liu Xiaoming, Hu Zhaochu, 2015. Chronology, Geochemistry and Hf Isotope of Granite from Southern Xingkai Block. Earth Science, 40(6): 982-994. doi: 10.3799/dqkx.2015.082

Citation:

Jing Haixin, Sun Deyou, Gou Jun, Wu Pengfei, Wang Tianhao, Guo Hongyu, Liu Xiaoming, Hu Zhaochu, 2015. Chronology, Geochemistry and Hf Isotope of Granite from Southern Xingkai Block. Earth Science, 40(6): 982-994. doi: 10.3799/dqkx.2015.082

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Chronology, Geochemistry and Hf Isotope of Granite from Southern Xingkai Block

doi: 10.3799/dqkx.2015.082

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
State Key Laboratory of Continental Dynamics, Northwest University, Xi'an 710069, China
3.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2014-12-24
Publish Date: 2015-06-15

Abstract

Abstract

The tectonic evolution of southern Khanka block is very complex, and there is not enough of the precise chronological evidence and systematic geochemical studies. Zircon U-Pb dating results show that the granites from southern Xingkai block were intruded at the end of Late Triassic (202-205 Ma) in a transition stage of paleo-Asian Ocean and paleo-Pacific tectonic system. It is found that the monzonitic granites and granodiorites are all characterized with enriched silicon (SiO₂=69.61%-77.27%), weakly supersaturated aluminum (Al₂O₃=12.70%-15.28%) and relatively enriched potassium (AKI=0.64-0.88), which indicates that the granites are fractionated Ⅰ-type granites, taking into account of the presence of amphibole and low zircon saturation temperature (T_Zr=679-787 ℃). ¹⁷⁶Hf/¹⁷⁷Hf ratios are high (0.282 773-0.282 913); ε_Hf(t) is positive (4.39-9.32), and two-stage Hf model ages are young (0.65-0.96 Ga), which shows that its source material is from the depleted mantle of new-born young crust of Neoproterozoic. It is concluded that the granite was formed in the context of the initial western Pacific subduction into active continental margin based on the age of the rock formation, and other rock features.
- granite,
- U-Pb dating,
- geochronology,
- geochemistry,
- Xingkai block

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References(47)

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