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Research on Sequence Stratigraphy of Nantun Formation in Bayanhushu Depression of Hailar Basin and Favorable Target

机译:海伦盆地北屯坳陷南屯形成序列地层研究及良好目标

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Exploration in Bayanhushu depression has been published from time to time,showing great exploration potential,but the degree is low at present.We devided Nantun formation into two third sequences through comprehensive analysis and studied on the types and distribution of sedimentary facies.The conclusion shows that Nantun formation is mainly comprised of fan delta,braid delta and lacustrine facies.The fan delta sedimentary facies mainly distribute in the western steep slope zone,while the braided river delta develops in the eastern gentle slope zone,and the lacustrine facies mainly develops in the middle trough zone and the edge of the fan delta.The sedimentary pattern has the characteristics of"east-west zoning".From the steep slope to the gentle slope,the types of sedimentary facies gradually change from fan delta to shore-shallow lake,semi-deep lake to deep lake and then to braided river delta.The study of source-reservoir-cap assemblages and accumulation conditions shows that fan delta front and braided delta front have good physical properties and are close to high grade source.So it is easy to form inversion structural reservoirs in the steep slope break zone,while fault-lithologic reservoirs in gentle slope zone,a lithologic reservoirs near trough areas.
机译:巴彦州坳陷勘探已不时发布,展现出巨大的勘探潜力,但目前较低。我们通过综合分析将南屯形成分为两个第三个序列,并研究了沉积相的类型和分布。结论显示芬屯形成主要由粉丝三角洲和湖泊和湖泊面积组成。范三角洲沉积相主要分布在西方陡坡区,而编织河三角洲在东部温柔的坡度发展,湖泊面主要发展中间槽区和粉丝三角洲的边缘。沉积图案具有“东西西区分区”的特点。从陡坡到温柔的坡度,沉积面的类型逐渐从粉丝三角到岸浅湖,半深湖到深湖,然后到编织河三角洲。源 - 储层帽组合和累积条件的研究表明,风扇D Elta Front和Raided Delta Front具有良好的物理性质,靠近高品位来源。所以,在陡坡断裂区中易于形成反转结构储层,而温柔斜坡区的故障岩性水库,岩石区附近的岩性水库。

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