Yanshanian metamorphism of Jiaodong Peninsula: New evidence from zircon and titanite U-Pb dating of (garnet) amphibolites in the Rushan area, Sulu tectonic complex belt

ZHANG Lianxiang; TIAN Zhonghua; LIU Pinghua; WEN Fei; ZHU Haozhong; ZHANG Chuanheng; YE Zhanghuang

2021 Vol. 40, No. 5

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ZHANG Lianxiang, TIAN Zhonghua, LIU Pinghua, WEN Fei, ZHU Haozhong, ZHANG Chuanheng, YE Zhanghuang. Yanshanian metamorphism of Jiaodong Peninsula: New evidence from zircon and titanite U-Pb dating of (garnet) amphibolites in the Rushan area, Sulu tectonic complex belt[J]. Geological Bulletin of China, 2021, 40(5): 674-686.

Citation:

ZHANG Lianxiang, TIAN Zhonghua, LIU Pinghua, WEN Fei, ZHU Haozhong, ZHANG Chuanheng, YE Zhanghuang. Yanshanian metamorphism of Jiaodong Peninsula: New evidence from zircon and titanite U-Pb dating of (garnet) amphibolites in the Rushan area, Sulu tectonic complex belt[J]. Geological Bulletin of China, 2021, 40(5): 674-686.

Yanshanian metamorphism of Jiaodong Peninsula: New evidence from zircon and titanite U-Pb dating of (garnet) amphibolites in the Rushan area, Sulu tectonic complex belt

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Department of Mineral Geology, School of Earth Sciences and Engineering, Shandong University of Science and Technology, Qingdao 266000, Shandong, China
4.
Jiangxi Science and Technology Normal University, Nanchang 330038, Jiangxi, China

More Information

Corresponding author: TIAN Zhonghua, tianzhonghua@cags.ac.cn

Received Date: 10 August 2020

Revised Date: 05 December 2020

Publish Date: 15 May 2021

Abstract

Abstract

The "Yanshanian Movement" generally refers to the large-scale tectonic movement of the eastern China in Jurassic-Cretaceous.Its related structural and magmatic events have been deeply studied by previous researchers.However, a few Yanshanian metamorphic ages were reported previously in the eastern China.In this study, LA-ICP-MS U-Pb dating of zircons and titanite from the(garnet) amphibolites in Rushan region indicates that: (1) the formation age of the Niantou garnet amphibolites was 1708 Ma, and the metamorphic age was 154 Ma; (2) the early metamorphic age of the Beizhuang amphibolite was 1840 Ma, and the late metamorphic age was 145 Ma.On the basis of the above new zircon and titanite age and the new magmatic-tectonic data of the Jiaodong Peninsula, it is suggested that the garnet amphibolites of the Rushan region have ever recorded the Yanshanian metamorphic event, and it is speculated that the metamorphic event occurred in a special period of regional tectonic transformation stage(from compression to extension), and the origin of the metamorphism may be related to the regional tectonic thickening during the Yanshanian orogeny in eastern China, but at present it cannot be ruled out that the metamorphism of this period is possibly related to the thermal drive of magmatism at the same time.
- Yanshanian movement /
- metamorphism /
- zircon and titanite U-Pb dating /
- Sulu tectonic complex belt

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