山东青岛地区灵山岛早白垩世碎屑岩锆石U-Pb-Hf同位素特征及其大地构造意义

孟元库; 李日辉; 徐扬; 侯方辉

doi:10.3799/dqkx.2018.207

Volume 43 Issue 9

Sep. 2018

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Article Navigation > Earth Science > 2018 > 43(9): 3302-3323

Meng Yuanku, Li Rihui, Xu Yang, Hou Fanghui, 2018. U-Pb-Hf Isotopes and Tectonic Significance of Early Cretaceous Detrital Zircons on Lingshan Island, Qingdao of Shandong Province. Earth Science, 43(9): 3302-3323. doi: 10.3799/dqkx.2018.207

Citation:

Meng Yuanku, Li Rihui, Xu Yang, Hou Fanghui, 2018. U-Pb-Hf Isotopes and Tectonic Significance of Early Cretaceous Detrital Zircons on Lingshan Island, Qingdao of Shandong Province. Earth Science, 43(9): 3302-3323. doi: 10.3799/dqkx.2018.207

Citation:

Meng Yuanku, Li Rihui, Xu Yang, Hou Fanghui, 2018. U-Pb-Hf Isotopes and Tectonic Significance of Early Cretaceous Detrital Zircons on Lingshan Island, Qingdao of Shandong Province. Earth Science, 43(9): 3302-3323. doi: 10.3799/dqkx.2018.207

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U-Pb-Hf Isotopes and Tectonic Significance of Early Cretaceous Detrital Zircons on Lingshan Island, Qingdao of Shandong Province

doi: 10.3799/dqkx.2018.207

Meng Yuanku^{1,2,3
,},
Li Rihui^{1,2
,
,},
Xu Yang^1,2,
Hou Fanghui^1,2

1.
Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, China
2.
Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China
3.
Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2018-01-08
Publish Date: 2018-09-15

Abstract

Abstract

The Early Cretaceous clastic rocks were deposited on Lingshan island, the eastern segment of the Sulu orogenic belt. However, the accurate depositional age, formation mechanism and tectonic setting of the Early Cretaceous clastic rocks are still controversial. In this study, we conducted systematically detrital zircon LA-ICP-MS U-Pb dating for two sets of clastic rocks on Lingshan island, and carried out Lu-Hf isotopic analyses for the representative detrital zircons. The results show as follows:(1) The detrital zircon U-Pb analyses demonstrate that the Fajiaying Formation and the clastic rocks from the bottom of the Bamudi Formation were deposited in the mid-late periods of Early Cretaceous, showing the synchronous depositional ages within the uncertainties, 127±3 Ma and 128±4 Ma, respectively. (2) Moreover, two sets of clastic rocks have the same age spectra and similar Hf isotopic compositions, indicating that the sandstone or mudstone characterized by soft sedimentary deformations and pebbly cearse sandstone have the similar sedimentary provenance, which was single and mainly derived from the Jiaobei terrane akin to the North China craton attributes, and then from the Sulu orogenic belt. (3) In comparison with the Jiaolai basin, the detrital zircons of the Laiyang Group in Lingshan island show different age spectra. We argue that the sedimentary rocks from Lingshan island might be deposited in an individual basin controlled by the fault different from the Jiaolai basin during Early Cretaceous. Integrated with previous studies, the Fajiaying Formation of the Laiyang Group on Lingshan island was possibly formed at the end of evolution of a lacustrine faulted-basin, and subsequently deposited a set of fluvial sediments characterized by pebbly sandstones at the top of the lacustrine sediments. Later on, the no-diagenetic sediments suffered from the strong volcanic earthquake, resulting in the soft sedimentary deformations and slump structures.
- detrital zircons U-Pb dating,
- the Early Cretaceous,
- sedimentary provenance,
- the Sulu orogenic belt,
- Lingshan island,
- isotope,
- geochronology

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References(125)

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