石臼坨凸起西南陡坡带扇三角洲锆石定年与源汇示踪

赵梦; 徐长贵; 杜晓峰; 王清斌

doi:10.3799/dqkx.2017.126

Volume 42 Issue 11

Nov. 2017

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Zhao Meng, Xu Changgui, Du Xiaofeng, Wang Qingbin, 2017. Detrital Zircon U-Pb Geochronology and Provenance Tracing of the Fan Deltas along the Southwestern Slope of the Shijiutuo Uplift. Earth Science, 42(11): 1984-1993. doi: 10.3799/dqkx.2017.126

Citation:

Zhao Meng, Xu Changgui, Du Xiaofeng, Wang Qingbin, 2017. Detrital Zircon U-Pb Geochronology and Provenance Tracing of the Fan Deltas along the Southwestern Slope of the Shijiutuo Uplift. Earth Science, 42(11): 1984-1993. doi: 10.3799/dqkx.2017.126

Citation:

Zhao Meng, Xu Changgui, Du Xiaofeng, Wang Qingbin, 2017. Detrital Zircon U-Pb Geochronology and Provenance Tracing of the Fan Deltas along the Southwestern Slope of the Shijiutuo Uplift. Earth Science, 42(11): 1984-1993. doi: 10.3799/dqkx.2017.126

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Detrital Zircon U-Pb Geochronology and Provenance Tracing of the Fan Deltas along the Southwestern Slope of the Shijiutuo Uplift

doi: 10.3799/dqkx.2017.126

Bohai Oilfield Research Institute, Tianjin Branch of China National Offshore Oil Corporation, Tianjin 300459, China

Received Date: 2017-02-17
Publish Date: 2017-11-15

Abstract

Abstract

To trace sedimentary Source-to-Sink systems of the southwestern Shijiutuo uplift, Bohai bay basin, 6 sandstone cuttings from 3 fan deltas of the third member of Dongying Formation (Ed₃), along the southwestern slope of Shijiutuo uplift, were systematically sampled for detrital zircon U-Pb dating analysis in this study. It is found that sediments of the western fan delta (C6-4-4) were characterized with abundant Cretaceous zircons and a notable peak at 110 Ma, controlled by volcanic rocks of Cretaceous Yixian Formation. The sediments of the middle fan delta (C6-4-3, C6-4-6D) and the eastern fan delta (C6-4-5D) were characterized by high percentage of Jurassic zircons and a 152 Ma or 168 Ma peak, dominated by volcanic rocks of Jurassic Lanqi Formation, while their Paleozoic zircons derived from the Mesozoic sedimentary rocks. Moreover, all the samples received Archean-Proterozoic zircons from the exposed basement. This study shows that all the source strata can be traced by detrital zircon U-Pb dating except for the Paleozoic carbonate. The diversity of the provenances of the fan deltas was controlled by the inclination of the source strata:as the Mesozoic strata inclined to northwest, the Cretaceous strata dominated the western fan delta while the Jurassic strata controlled the middle and eastern fan deltas.
- provenance,
- detrital zircon U-Pb age,
- the Cretaceous Yixian Formation,
- the Jurassic Lanqi Formation,
- the Shijiutuo uplift,
- sedimentary,
- petroleum geology

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Detrital Zircon U-Pb Geochronology and Provenance Tracing of the Fan Deltas along the Southwestern Slope of the Shijiutuo Uplift

doi: 10.3799/dqkx.2017.126

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