Age, Geochemistry, and Tectonic Implications of Dulaerqiao Granite, Inner Mongolia

Anxia Chen; Duo Zhou; Qingkui Zhang; Zhongzhu Yang

doi:10.1007/s12583-017-0817-6

Volume 29 Issue 1

Jan 2018

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Journal of Earth Science > 2018 > 29(1): 78-92.

Anxia Chen, Duo Zhou, Qingkui Zhang, Zhongzhu Yang. Age, Geochemistry, and Tectonic Implications of Dulaerqiao Granite, Inner Mongolia. Journal of Earth Science, 2018, 29(1): 78-92. doi: 10.1007/s12583-017-0817-6

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Anxia Chen, Duo Zhou, Qingkui Zhang, Zhongzhu Yang. Age, Geochemistry, and Tectonic Implications of Dulaerqiao Granite, Inner Mongolia. Journal of Earth Science, 2018, 29(1): 78-92. doi: 10.1007/s12583-017-0817-6

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Age, Geochemistry, and Tectonic Implications of Dulaerqiao Granite, Inner Mongolia

doi: 10.1007/s12583-017-0817-6

1.
Ocean College, Zhejiang University, Zhoushan 316021, China
2.
Liaoning Institute of Geological Exploration, Dalian 116100, China
3.
Shenyang Center, China Geological Survey, Shenyang 110032, China

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Corresponding author: Anxia Chen, chenanxia872006@126.com
Received Date: 17 May 2017
Accepted Date: 27 Sep 2017
Publish Date: 01 Feb 2018

Abstract

Abstract

Dulaerqiao granite is located at the Xinlin-Xiguitu-Toudaoqiao suture zone between the Erguna massif and the Xing'an massif, northeast of Inner Mongolia. The rocks are mainly composed of K-feldspar, quartz, and plagioclase. Zircon LA-ICP-MS U-Pb data show that this granite was deposited in the Late Carboniferous Period (308.7±2.0 Ma). The samples are rich in alkali, Fe, and Al and low in Mg, Ca, and P. Chondrite-normalized REEs exhibit right-inclined patterns with significant negative Eu anomalies. Additionally, the granite shows high quantities of trace elements such as Zr, Hf, Th, K, and Rb and decreased quantities of Sr, P, and Ti. The chemical characteristics identified herein and a series of diagrams that distinguish different types of granite show that Dulaerqiao alkali-feldspar granites belong to the aluminous A-type granite group. Meanwhile, the initial magma crystallizes under high-temperature, low-pressure conditions resulting from a tectonic extension setting. The formation of Dulaerqiao aluminous A-type granite is related to the rejuvenation of the ancient Xinlin-Xiguitu-Toudaoqiao suture zone, which was activated by the interaction between the combined Erguna-Xing'an massif and the Songnen massif in the Late Paleozoic Era. This aluminous A-type granite was deposited about 30 Ma after the collision.
- aluminous A-type granite,
- zircon U-Pb age,
- geochemistry,
- post-orogenic extensional environment,
- rejuvenation of an ancient suture zone,
- Dulaerqiao

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References(87)

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Age, Geochemistry, and Tectonic Implications of Dulaerqiao Granite, Inner Mongolia

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Age, Geochemistry, and Tectonic Implications of Dulaerqiao Granite, Inner Mongolia

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