渤海湾盆地车西洼陷陡坡带古近系沙河街组沙三下段“源-汇”系统

doi:10.7605/gdlxb.2016.01.005

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Abstract

Based on core observation, well logs and 3-D seismic data, the research in the “source-to-sink” system of the Lower Member 3 of Paleogene Shahejie Formation in the steep slope zone of Western Chezhen sub-sag of Chezhen sag, Bohai Bay Basin, is conducted. The results show that:(1)The Lower Member 3 of Shahejie Formation is a third-order sequence which can be divided into three system tracts, including the lowstand system tract, transgressive system tract and highstand system tract, and in the steep slope zone, 11 gravity flow rock types and deep-lacustrine mudstone can be identified,and the gravity flow rock types include matrix-supported medium-grained conglomerates,clast-supported medium-grained conglomerates,matrix-supported fine-grained conglomerates,clast-supported fine-grained conglomerates,sandy conglomerate,conglomeratic sandstones,coarse sandstones,medium sandstones,fine sandstones,graded bedding sandstones and slumps,they are all the typical characteristics of the near-shore subaqueous fan. The evolution tendency of fan scales is from increasing to decreasing,and then increasing again as a whole. (2)Six provenance supplying systems can be identified in the steep slope zone of Western Chezhen sub-sag,and they can be divided into two types,namely,gully-dominated provenance supplying systems and slump-dominated provenance supplying system. The slump structure are much more widely developed in the fans associated with the slump-dominated provenance supplying systems than the fans associated with the gully-dominated provenance supplying systems,in addition,the scale of slump near-shore subaqueous fans is smaller than the fans associated with gully. (3)The further study on the “source”area’s characteristics shows that,the parent rock developed in the depositional period of the Lower Member 3 of Shahejie Formation of the source area was mainly the carbonate rocks; under the action of strong tectonic activities and warm-wet climate,the source area may developed stony desertification palaeogeomorphology and strong erosion,which would cause frequent seasonal gravity to be transported into the lacustrine and form the near-shore subaqueous fans; the scale difference of the fans developed in different system tracts were mainly controlled by the climatic variation and vegetation cover of the source area.

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	Wang Xingxing
	Zhu Xiaomin
	Song Shuang
	Wu Chenbingjie
	He Jingcong
	Cao Gang

Key words： &#x0201c source-to-sink&#x0201d system Lower Member 3 of Shahejie Formation steep slope zone Western Chezhen sub-sag Chezhen sag Bohai Bay Basin

Received: 10 April 2015 Published: 01 February 2016

ZTFLH:

P531

Fund:

Co-funded by the subproject of National Significant Petroleum Special Projects of China(No.2011ZX05009-002, No.2012ZX05001-002), the National Natural Science Foundation of China(No.41272133) and the Young Scientists Foundation of National Natural Science Foundation of China(No.41202107)]

Cite this article:

Wang Xingxing,Zhu Xiaomin,Song Shuang et al. “Source-to-sink” system of the Lower Member 3 of Paleogene Shahejie Formation in steep slope zone of Western Chezhen sub-sag, Bohai Bay Basin[J]. JOPC, 2016, 18(1): 65-79.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2016.01.005 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2016/V18/I1/65

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