珠江口盆地惠州凹陷古近纪多幕裂陷旋回的沉积物源响应

王维; 叶加仁; 杨香华; 施和生; 舒誉; 吴静

doi:10.3799/dqkx.2015.088

Volume 40 Issue 6

Jun. 2015

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Wang Wei, Ye Jiaren, Yang Xianghua, Shi Hesheng, Shu Yu, Wu Jing, 2015. Sediment Provenance and Depositional Response to Multistage Rifting, Paleogene, Huizhou Depression, Pearl River Mouth Basin. Earth Science, 40(6): 1061-1071. doi: 10.3799/dqkx.2015.088

Citation:

Wang Wei, Ye Jiaren, Yang Xianghua, Shi Hesheng, Shu Yu, Wu Jing, 2015. Sediment Provenance and Depositional Response to Multistage Rifting, Paleogene, Huizhou Depression, Pearl River Mouth Basin. Earth Science, 40(6): 1061-1071. doi: 10.3799/dqkx.2015.088

Citation:

Wang Wei, Ye Jiaren, Yang Xianghua, Shi Hesheng, Shu Yu, Wu Jing, 2015. Sediment Provenance and Depositional Response to Multistage Rifting, Paleogene, Huizhou Depression, Pearl River Mouth Basin. Earth Science, 40(6): 1061-1071. doi: 10.3799/dqkx.2015.088

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Sediment Provenance and Depositional Response to Multistage Rifting, Paleogene, Huizhou Depression, Pearl River Mouth Basin

doi: 10.3799/dqkx.2015.088

Wang Wei^{1, 2
,},
Ye Jiaren^{1, 2},
Yang Xianghua^{1, 2
,
,},
Shi Hesheng³,
Shu Yu³,
Wu Jing³

1.
Key Laboratory of Tectonics and Petroleum Resources of the Ministry of Education, China University of Geosciences, Wuhan430074, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan430074, China
3.
CNOOC China Ltd., Shenzhen, Guangzhou510240, China

Received Date: 2015-01-22
Publish Date: 2015-06-15

Abstract

Abstract

In order to clarify the controlling effects of tectonic activities on the sediment supply and sedimentary filling, the sediment supply of the Huizhou depression is quantitatively studied by analyzing the changes in the shape and chronology of the detrital zircons of eight samples from different formations, with LA-ICPMS zircon U-Pb dating as the main measuring method. The southern provenance areas, Dongsha Massif and the internal uplifts of the basin, are predominantly composed of Mesozoic igneous rocks, while northern provenance areas, South China folded belt, are characterized by complicated lithology and geochronology. The results show that the content of Mesozoic zircon grains decreases while that of Precambrian-Paleozoic zircon grains increases and then prevails gradually from the Lower Wenchang Formation to the Upper Wenchang Formation and to the Enping Formation, confirming that the area provenance system switched a south provenance in the basin to a north provenance out of the basin gradually. The evolution of Huizhou depression in Paleogene can be divided into three rifted stages: periods Ⅰ_A, Ⅰ_B and Ⅱ. During period Ⅰ_A (Lower Wenchang Formation), the southern faults of depression suffered strong activities. All zircon grains are derived from Mesozoic, indicating sediments derived from the southern provenance areas. The related sedimentary facies are characterized by fan delta and middle-deep lake under the conditions of southern steep slope of Huizhou depression. During period I_B, corresponding to Upper Wenchang Formation, the tectonic activities are characterized by high subsidence rates in the northern fault zones. The content of Mesozoic grains is 68%, whereas the content of Precambrian-Paleozoic zircon grains is up to 32%, which indicates that sediments are derived from both northern and southern provenance areas. The related sedimentary facies have the characteristics of fan delta, braided river delta and middle-deep lake. During period Ⅱ (Enping Formation), the northern faults stayed active. The content of Precambrian-Paleozoic zircon grains increases to 64% while that of Mesozoic grains decreases to 36%, which indicates that northern provenance areas play a dominant role in this stage. In addition, the related sedimentary facies are characterized by shallower braided river delta, beach bar and thin coal seam.
- Huizhou depression,
- multistage rifting,
- provenance switching,
- zircon U-Pb dating,
- sediments,
- geochronology

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References(52)

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Sediment Provenance and Depositional Response to Multistage Rifting, Paleogene, Huizhou Depression, Pearl River Mouth Basin

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