海南岛东南海域碎屑锆石年代学物源示踪及构造指示意义

刘松峰; 李顺; 聂鑫; 邹俪琦; 蔡观强

doi:10.3799/dqkx.2021.024

Volume 46 Issue 11

Nov. 2021

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Article Navigation > Earth Science > 2021 > 46(11): 4084-4096

Liu Songfeng, Li Shun, Nie Xin, Zou Liqi, Cai Guanqiang, 2021. Detrital Zircon Geochronology from Southeastern Sea of Hainan Island: Provenance Tracing and Tectonic Implications. Earth Science, 46(11): 4084-4096. doi: 10.3799/dqkx.2021.024

Citation:

Liu Songfeng, Li Shun, Nie Xin, Zou Liqi, Cai Guanqiang, 2021. Detrital Zircon Geochronology from Southeastern Sea of Hainan Island: Provenance Tracing and Tectonic Implications. Earth Science, 46(11): 4084-4096. doi: 10.3799/dqkx.2021.024

Citation:

Liu Songfeng, Li Shun, Nie Xin, Zou Liqi, Cai Guanqiang, 2021. Detrital Zircon Geochronology from Southeastern Sea of Hainan Island: Provenance Tracing and Tectonic Implications. Earth Science, 46(11): 4084-4096. doi: 10.3799/dqkx.2021.024

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Detrital Zircon Geochronology from Southeastern Sea of Hainan Island: Provenance Tracing and Tectonic Implications

doi: 10.3799/dqkx.2021.024

Liu Songfeng^{1, 2, 3
,
,},
Li Shun^{1, 3},
Nie Xin^{1, 3},
Zou Liqi^{1, 2},
Cai Guanqiang^{1, 2, 3
,
,
,}

1.
Guangzhou Marine Geological Survey, China Geological Survey, Ministry of Natural Resources, Guangzhou 510760, China
2.
Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou 510075, China
3.
Southern Marine Science and Engineering Guangdong Laboratory, Guangzhou 511458, China

Received Date: 2021-02-08
Available Online: 2021-12-04
Publish Date: 2021-11-30

Abstract

Abstract

In order to explore the provenance of surface sediments in the southeastern sea of Hainan Island and reveal the evolution history of major geological tectonic events in the provenance area, it used the box corer method to obtain sediment samples from 8 stations, and zircon U-Pb dating analyses were performed. The results show that 773 effective ages are distributed between 33 and 3 205 Ma, and the main age peaks are concentrated in the Yanshanian (100 Ma, 140 Ma and 159 Ma), Indosinian (242 Ma) and Caledonian (439 Ma). The secondary age peaks are concentrated in the Neoproterozoic (776 Ma, 965 Ma) and Paleoproterozoic (1 836 Ma, 2 487 Ma), and the Archean basement age information is scattered. A small number of metamorphic zircons records strong metamorphic events in the Caledonian and Indosinian. A comparative analysis with potential provenance area shows that the sediments in the southeastern sea of Hainan Island are identified by the age peak of about 100 Ma, which are mainly from Hainan Island. Combined with previous studies, the age spectrum in this study indicates that the Caledonian Wuyi-Yunkai orogenic belt in Cathaysia can extend to Hainan Island, the closure of the Paleo-Tethys Ocean and the collision between the Indosinian and Cathaysia blocks in Hercynian-Indosinian led to its strong tectonism-magmatism-metamorphism, and Hainan Island developed multiple magmatic activities due to the subduction of the Pacific plate in the Yanshanian.
- southeastern sea of Hainan Island,
- sediment,
- detrital zircon,
- provenance tracing,
- geological evolution,
- tectonics

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References(66)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Detrital Zircon Geochronology from Southeastern Sea of Hainan Island: Provenance Tracing and Tectonic Implications

doi: 10.3799/dqkx.2021.024

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通讯作者: 陈斌, bchen63@163.com

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