扬子克拉通北缘新元古代A型花岗岩的发现及大地构造意义

曹正琦; 蔡逸涛; 曾佐勋; 胡正祥; 陈静; 蒋幸福; 孙政权; 吴波; 刘成新; 郭盼

doi:10.3799/dqkx.2017.80

Volume 42 Issue 6

Jun. 2017

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Article Navigation > Earth Science > 2017 > 42(6): 957-943

Cao Zhengqi, Cai Yitao, Zeng Zuoxun, Hu Zhengxiang, Chen Jing, Jiang Xingfu, Sun Zhengquan, Wu Bo, Liu Chengxin, Guo Pan, 2017. Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance. Earth Science, 42(6): 957-943. doi: 10.3799/dqkx.2017.80

Citation:

Cao Zhengqi, Cai Yitao, Zeng Zuoxun, Hu Zhengxiang, Chen Jing, Jiang Xingfu, Sun Zhengquan, Wu Bo, Liu Chengxin, Guo Pan, 2017. Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance. Earth Science, 42(6): 957-943. doi: 10.3799/dqkx.2017.80

Citation:

Cao Zhengqi, Cai Yitao, Zeng Zuoxun, Hu Zhengxiang, Chen Jing, Jiang Xingfu, Sun Zhengquan, Wu Bo, Liu Chengxin, Guo Pan, 2017. Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance. Earth Science, 42(6): 957-943. doi: 10.3799/dqkx.2017.80

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Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance

doi: 10.3799/dqkx.2017.80

1.
School of Earth Sciences, China University of Geosciences, Wuhan430074, China
2.
Hubei Institute of Geological Survey, Wuhan430034, China
3.
Nanjing Geological Survey Center, China Geological Survey, Nanjing210016, China
4.
College of Earth Sciences, East China Institute of Technology, Nanchang330013, China

Received Date: 2016-12-10
Publish Date: 2017-06-15

Abstract

Abstract

Researches on the Daleishan gneissic granites can constrain Neoproterozoic Rodinia supercontinent breakup in the northern margin of Yangtze craton. In this paper, zircon U-Pb dating, in-situ Lu-Hf isotope and whole-rock geochemical compositions analyses are presented for the Daleishan gneissic granites in the northern margin of the Yangtze craton. The results show that the Daleishan gneissic granites have high contents of SiO₂ (73.18%-77.40%) and alkali (8.07%-8.70%), but low contents of Al₂O₃ (12.11%-13.92%) and MgO (0.10%-0.34%), and display enrichment in Ga, Rb, Th, Zr, Hf but depletion in Nb, Sr, P, Ti, which indicates the post-orogenic A-type affinity. Zircons selected from two Daleishan gneissic granitic samples show typical oscillatory zone structure with high ratios of Th/U (greater than 0.5), exhibiting the magmatic zircon genesis. LA-ICP-MS (laser ablation inductively coupled plasma mass spectrometry) zircon U-Pb data from the two samples yield Neoproterozoic crystallization ages of 801.3±3.0 Ma (MSWD=0.62) and 796.1±6.3 Ma (MSWD=1.70), respectively, which are interpreted to represent the intrusion time. In-situ Hf isotopic compositions show that the two gneissic granitic samples have wide range of ε_Hf(t) values that are indicative of a heterogeneity property. ε_Hf(t) values of these zircon ranges from -7.5 to +8.0, with the positive ε_Hf(t) values, coinciding with the single phase model age (t_DM1) of the depleted mantle of (1 242-1 059 Ma), and the negative ε_Hf(t) values coinciding with two-phase model age (t_DM2) of the crustal of (1 636-1 981 Ma), suggesting that the oldest existing material in the region belongs to Paleoproterozoic (as old as 1 981 Ma). These data show that the source materials of the Daleishan A-type granites were usually derived from Palaeoproterozoic ancient crust. The magmatic source of the granites was originated from the crust-mantle migmatization, and the mantle composition could have been generated from the upwelling of the mantle magma in the extensional background. Combining with the pre-existing regional publications, it is proposed that the Daleishan A-type granite was formed at the crustal extensional background in the continental back-arc setting associated with the assembly-break up process of the Rodinia supercontinent.
- northern margin of Yangtze craton,
- Neoproterozoic,
- A-type granite,
- zircon U-Pb dating,
- Lu-Hf isotopic composition,
- petrology

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References(82)

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Discovery of Neoproterozoic A-Type Granite in Northern Yangtze Craton and Its Tectonic Significance

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