内蒙古朱日和地区早古生代岩浆岩年代学、地球化学特征及其构造意义

钱筱嫣; 张志诚; 陈彦; 于海飞; 罗志文; 杨金福

doi:10.3799/dqkx.2017.545

Volume 42 Issue 9

Sep. 2017

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Qian Xiaoyan, Zhang Zhicheng, Chen Yan, Yu Haifei, Luo Zhiwen, Yang Jinfu, 2017. Geochronology and Geochemistry of Early Paleozoic Igneous Rocks in Zhurihe Area, Inner Mongolia and Their Tectonic Significance. Earth Science, 42(9): 1472-1494. doi: 10.3799/dqkx.2017.545

Citation:

Qian Xiaoyan, Zhang Zhicheng, Chen Yan, Yu Haifei, Luo Zhiwen, Yang Jinfu, 2017. Geochronology and Geochemistry of Early Paleozoic Igneous Rocks in Zhurihe Area, Inner Mongolia and Their Tectonic Significance. Earth Science, 42(9): 1472-1494. doi: 10.3799/dqkx.2017.545

Citation:

Qian Xiaoyan, Zhang Zhicheng, Chen Yan, Yu Haifei, Luo Zhiwen, Yang Jinfu, 2017. Geochronology and Geochemistry of Early Paleozoic Igneous Rocks in Zhurihe Area, Inner Mongolia and Their Tectonic Significance. Earth Science, 42(9): 1472-1494. doi: 10.3799/dqkx.2017.545

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Geochronology and Geochemistry of Early Paleozoic Igneous Rocks in Zhurihe Area, Inner Mongolia and Their Tectonic Significance

doi: 10.3799/dqkx.2017.545

Qian Xiaoyan^{1,2
,},
Zhang Zhicheng^{1,2
,
,},
Chen Yan^1,2,
Yu Haifei^1,2,
Luo Zhiwen^1,2,
Yang Jinfu^1,2

1.
Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, Peking University, Beijing 100871, China
2.
School of Earth and Space Sciences, Peking University, Beijing 100871, China

Received Date: 2016-12-28
Publish Date: 2017-09-15

Abstract

Abstract

There are some existing debates about the tectonic history of the Central Asian Orogenic Belt, including the time of collision.New zircon SHRIMP and LA-ICP-MS U-Pb isotopic data, zircon Lu-Hf isotopic data and geochemical data of the volcanic rocks and plutons from the Eerdengtaolegai area are presented to study their formation ages and petrogenesis.Zircon U-Pb ages of 432.8±2.6 Ma, 428.1±1.8 Ma of Silurian granites, 434.0±4.4 Ma of Silurian dacite, 411.8±1.0 Ma of the Devonian rhyolite were obtained.The Silurian plutons are mostly intermediate-acid rocks, and are geochemically low in K contents, peraluminous, and calc-alkaline with enrichment in Rb and Th and depletion in Nb, Ta, P and Ti.They do not have negative Eu anomalies. Two granites from these plutonic rocks have positive ε_Hf(t) values (-1.19 to 11.51 and 3.32 to 10.28) with T_MD2 of 684-1 493 Ma and 759-1 202 Ma, suggesting that the granites may come from a juvenile continental crust.Geochemically, the Silurian volcanic rocks, all acid rocks, are low to moderate in K content, metaluminous-peraluminous and calc-alkaline with enrichment in Rb, Th and depletion in Nb, Ta, P and Ti.In addition, they do net have negative Eu anomalies. One Silurian dacite has positive ε_Hf(t) value (3.70-7.94) with T_MD2 of 912-1 183 Ma, suggesting that the rocks may come from the juvenile continental crust.The Devonian rhyolite have clear negative Eu anomalies, exhibiting negative ε_Hf(t) values (-14.95 to -7.07) with Hf model ages (T_MD2) of 1.8-2.3 Ga, indicating considerable contribution of reworked materials from the ancient crust of the North China Craton.Based on our new data and previous studies, the Silurian granites and dacite were likely formed in an arc environment and the Devonian rhyolite developed in a post-collisional environment.
- Inner Mongolia,
- Eerdengtaolegai,
- Bainaimiao,
- geochronology,
- geochemistry,
- Hf isotope

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References(97)

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Geochronology and Geochemistry of Early Paleozoic Igneous Rocks in Zhurihe Area, Inner Mongolia and Their Tectonic Significance

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