胶莱盆地蛇窝泊地区白垩纪林寺山组沉积时代与物源特征：来自碎屑锆石U-Pb测年与稀土元素组成的新证据

张连祥; 刘平华; 王义龙; 周万蓬; 张宇佳; 张传恒

doi:10.3799/dqkx.2020.403

Volume 46 Issue 3

Mar. 2021

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Zhang Lianxiang, Liu Pinghua, Wang Yilong, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Depositional Timing and Provenance Characteristics of the Cretaceous insishan Formation in the Shewopo Area, Jiaolai Basin: New Evidence from Detrital Zircon U-Pb Dating and REE Composition. Earth Science, 46(3): 1119-1132. doi: 10.3799/dqkx.2020.403

Citation:

Zhang Lianxiang, Liu Pinghua, Wang Yilong, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Depositional Timing and Provenance Characteristics of the Cretaceous insishan Formation in the Shewopo Area, Jiaolai Basin: New Evidence from Detrital Zircon U-Pb Dating and REE Composition. Earth Science, 46(3): 1119-1132. doi: 10.3799/dqkx.2020.403

Citation:

Zhang Lianxiang, Liu Pinghua, Wang Yilong, Zhou Wanpeng, Zhang Yujia, Zhang Chuanheng, 2021. Depositional Timing and Provenance Characteristics of the Cretaceous insishan Formation in the Shewopo Area, Jiaolai Basin: New Evidence from Detrital Zircon U-Pb Dating and REE Composition. Earth Science, 46(3): 1119-1132. doi: 10.3799/dqkx.2020.403

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Depositional Timing and Provenance Characteristics of the Cretaceous insishan Formation in the Shewopo Area, Jiaolai Basin: New Evidence from Detrital Zircon U-Pb Dating and REE Composition

doi: 10.3799/dqkx.2020.403

Zhang Lianxiang^{1, 2
,
,},
Liu Pinghua^{2
,
,
,},
Wang Yilong^{3, 2},
Zhou Wanpeng³,
Zhang Yujia^{3, 2},
Zhang Chuanheng¹

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.
School of Earth Sciences, East China University of Technology, Nanchang 330013, China

Received Date: 2020-12-16
Publish Date: 2021-03-15

Abstract

Abstract

Linsishan Formation is one of the important stratigraphic units at the bottom of the Early Cretaceous Laiyang Group in the Jiaolai basin. The accurate determination of depositional timing and provenance characteristics of the Linsishan Formation is of great importance for the objective reconstruction of the Late Mesozoic tectonic framework in the eastern part of the North China Block and the Late Mesozoic exhumation process of the surrounding orogenic belt/Precambrian basement. In this paper, we present an integrated study involving detailed field geological investigation, petrographic observation, zircon and U-Pb dating and in situ trace element analysis of the fine-grade conglomerates from the Linsishan Formation in the Laiyang Group, and the following conclusions are suggested: (1) The weighted mean age of the youngest group of detrital zircons in the fine-grade conglomerates of Linsishan Formation are 129±1 Ma and 127±5 Ma, combining with the zircon concordant age of 119±1 Ma yielded by magmatic zircons in the volcanic rocks from the Qingshan Group. It is speculated that the depositional timing of the Linsishan Formation in the Shewopo area is 127-119 Ma. (2) The detrital zircon ages of the fine-grade conglomerate of the Linsishan Formation in the Shewopo area range from 2 858 to 126 Ma, respectively, and are marked by the occurrence of the Late Neoarchean and Early Cretaceous ages. The pre-Paleoproterozoic detrital zircons are mainly derived from Precambrian metamorphic rocks of the Jiaobei terrane, indicating that the Archean-Paleoproterozoic metamorphic rocks of the Jiaobei terrane have exhumated to the near surface at least in the Early Cretaceous. (3) The 160-120 Ma magmatic detrital zircons are mainly derived from the synchronous intermediate acid intrusions in Jiaodong, suggesting that at least part of the 160-120 Ma intermediate acid intrusions have returned to the surface during the Early Cretaceous. (4) Permian (280 Ma) and Late-Triassic (213 Ma) metamorphic zircons which are identified in the Linsishan Formation, not only indicate that the Late Paleozoic (280 Ma) metamorphic event may have occurred in Jiaodong Peninsula, and but also reveal that Sulu UHP metamorphic rocks have exhumed to the surface during the Early Cretaceous.
- Jiaolai basin,
- Linsishan Formation,
- depositional timing,
- zircon U-Pb dating,
- petrology

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References(76)

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Depositional Timing and Provenance Characteristics of the Cretaceous insishan Formation in the Shewopo Area, Jiaolai Basin: New Evidence from Detrital Zircon U-Pb Dating and REE Composition

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