辽东岫岩地区两类古元古代花岗岩年代学、地球化学及地质意义

赵岩; 张朋; 毕中伟; 杨中柱; 寇林林; 顾玉超; 杨凤超

doi:10.3799/dqkx.2020.218

Volume 45 Issue 11

Nov. 2020

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Zhao Yan, Zhang Peng, Bi Zhongwei, Yang Zhongzhu, Kou Linlin, Gu Yuchao, Yang Fengchao, 2020. Geochronology and Geochemistry of Two Types of Paleoproterozoic Granites and Their Geological Implications in the Xiuyan Area, Liaodong Peninsula. Earth Science, 45(11): 4072-4090. doi: 10.3799/dqkx.2020.218

Citation:

Zhao Yan, Zhang Peng, Bi Zhongwei, Yang Zhongzhu, Kou Linlin, Gu Yuchao, Yang Fengchao, 2020. Geochronology and Geochemistry of Two Types of Paleoproterozoic Granites and Their Geological Implications in the Xiuyan Area, Liaodong Peninsula. Earth Science, 45(11): 4072-4090. doi: 10.3799/dqkx.2020.218

Citation:

Zhao Yan, Zhang Peng, Bi Zhongwei, Yang Zhongzhu, Kou Linlin, Gu Yuchao, Yang Fengchao, 2020. Geochronology and Geochemistry of Two Types of Paleoproterozoic Granites and Their Geological Implications in the Xiuyan Area, Liaodong Peninsula. Earth Science, 45(11): 4072-4090. doi: 10.3799/dqkx.2020.218

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Geochronology and Geochemistry of Two Types of Paleoproterozoic Granites and Their Geological Implications in the Xiuyan Area, Liaodong Peninsula

doi: 10.3799/dqkx.2020.218

Zhao Yan^{1, 2
,},
Zhang Peng^{1, 2},
Bi Zhongwei^{1, 2},
Yang Zhongzhu^{1, 2
,
,},
Kou Linlin^{1, 2},
Gu Yuchao^{1, 2},
Yang Fengchao^{1, 2}

1.
Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China
2.
Northeast Science & Technology Innovation Center, China Geological Survey, Shenyang 110034, China

Received Date: 2020-05-15
Publish Date: 2020-11-15

Abstract

Abstract

The Xiuyan region in Liaodong Peninsula is an ideal place for studying early evolution process of the Jiao-Liao-Ji orogenic belt, due to quantities of outcropped meta-sidimentary rocks and granitoids. A study of petrography, geochemistry and chronology is carried out on one K-feldspar granite, two mozogranite and one granodiorite samples collected from the Dafangshen, Muniu, Songshugou and Simenzi intrusions respectively. Although the K-feldspar granite and mozogranite samples show different features by petrography observation, they display similar geochemical natures of A-type granite. The samples have high contents of SiO₂, ranging from 70.56% to 74.52%, relatively low Al₂O₃ contents of 11.85% to 14.03%, and high ratio of K₂O/Na₂O, with enrichment of Ga, Zr and REE elements and depletion of Sr, P and Ti. The granodiorite sample from the Simenzi intrusion, on the other hand, shows characteristics of I-type granite. They have high content of CaO (0.50%-3.76%), but low ratio of K₂O/Na₂O and A/CNK, with relative depletion of some high field strength elements like Nb, Ta and Hf. Zircon LA-ICP-MS testing also reveals these granitoids intruded nearly simultaneously, with the K-feldspar granite sample yielding an U-Pb age of 2 198±11 Ma, mozogranite samples yielding U-Pb ages between 2 171-2 167 Ma and granodiorite sample giving an U-Pb age of 2 166±11 Ma. The I-type granite may have derived from an arc magmatism in middle Paleoproterozoic (about 2.2-2.1 Ga), while the A-type granitoids intrusions may have sourced from a low pressure and high temperature environment of middle to lower crust partial melting. Taking previous studies on Paleoproterozoic granitoids into consideration, the K-feldspar granite and mozogranite intrusions are believed to be formed under a back-arc geodynamic setting. An arc-continent collison model is confirmed in middle stage of the Paleoproterozoic Jiao-Liao-Ji belt evolution, and the subduction of early ocean crust may have started by then from west to east and have lasted a relatively long time.
- Jiao-Liao-Ji orogenic belt,
- granitoids,
- zircon U-Pb ages,
- arc-continent collison model,
- North China Craton,
- Xiuyan area,
- geochemistry

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Geochronology and Geochemistry of Two Types of Paleoproterozoic Granites and Their Geological Implications in the Xiuyan Area, Liaodong Peninsula

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