渤海湾盆地庙西北地区古近系沙河街组三段源-汇系统重建

doi:10.12108/yxyqc.20240308

Lithologic Reservoirs ›› 2024, Vol. 36 ›› Issue (3): 84-95.doi: 10.12108/yxyqc.20240308

• PETROLEUM EXPLORATION • Previous Articles

Reconstruction of source-to-sink system of the third member of Paleogene Shahejie Formation in Miaoxibei area，Bohai Bay Basin

FENG Bin¹, HUANG Xiaobo², HE Youbin¹, LI Hua¹, LUO Jinxiong¹, LI Tao¹, ZHOU Xiaoguang²

1. School of Geosciences, Yangtze University, Wuhan 430100, China;
2. Tianjin Branch of CNOOC, Tianjin 300452, China

Received:2023-07-10 Revised:2023-09-22 Published:2024-04-30

Abstract

Abstract: Based on drilling cores and 3D seismic data, the provenance characteristics and sedimentary facies distribution in Miaoxibei area in the Bohai Bay Basin were comprehensively analyzed from three aspects:source lithology identification, reconstruction of watershed river paleo-system and transport pathways, and the sourceto-sink system for the third member of Paleogene Shahejie Formation was reconstructed through the restoration of both paleo-geomorphological features within the sedimentary area and those within the denudation source area. The results show that:（1）A complete source-to-sink system of the third member of Paleogene Shahejie Formation has developed in Miaoxibei area, Bohai Bay Basin, with the provenance area located at Miaoxibei uplift and Bodong sag serving as the main sedimentary area. The source lithologies in Miaoxibei uplift comprise Mesozoic granite, Lower Proterozoic quartz schist, and Lower Proterozoic breccia. The primary watershed is distributed from south to north along the long axis of the uplift, with ancient water systems scattered within it. The main transport pathways consist of five ancient valleys and two ancient fault troughs. Fan delta-lacustrine facies deposits of the third member of Paleogene Shahejie Formation in Miaoxibei area are mainly characterized by rapid accumulation, mainly composed of gravel-bearing sandstone, fine sandstone and mudstone, with poor sorting and grinding degree. Rock composition and mineral association relatively match those found in quartz schist and granite located in Miaoxibei uplift. In northern Bodong sag, contiguous fan-shaped deltas dominate while isolated ones prevail in its southern part.（2）The denudation during the sedimentary period of Sha 3 member was pronounced in western Miaoxibei uplift and comparatively weaker in the eastern region, resulting in a gradual westward migration of the paleo-divide. The central and northern parts of Miaoxibei uplift exhibited a larger provenance area, significant vertical elevation differences, and a stronger supply capacity from the provenance. The thickness of the third member of Paleogene Shahejie Formation in Bodong sag varies between 100 to 600 m, with thinner deposits observed in the east and south, while thicker deposits are found in the west and north. The depositional center is located in the northern part of Bodong sag, where strata have undergone more extensive denudation reaching up to 3.2 km towards the east. The development location of fan delta is controlled by transport channels originating from provenance areas, while its scale is influenced by provenance size. Notably, fan delta deposition on a larger scale predominantly occurs in the northern and middle regions of Bodong sag which represent favorable areas for exploration.

Key words: source-to-sink system, watershed, ancient water system, paleogeomorphic restoration, fan delta, ancient valleys and ancient fault troughs, the third member of Shahejie Formation, Paleogene, Miaoxibei area, Bohai Bay Basin

CLC Number:

TE121.3

FENG Bin, HUANG Xiaobo, HE Youbin, LI Hua, LUO Jinxiong, LI Tao, ZHOU Xiaoguang. Reconstruction of source-to-sink system of the third member of Paleogene Shahejie Formation in Miaoxibei area，Bohai Bay Basin[J].Lithologic Reservoirs, 2024, 36(3): 84-95.

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Reconstruction of source-to-sink system of the third member of Paleogene Shahejie Formation in Miaoxibei area，Bohai Bay Basin

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