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Analysis of Braided River Deltaic Depositional System in the Eastern Sag of Liaohe Basin

机译:辽河盆地东部凹陷辫状河三角洲沉积体系分析

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According to the analysis of drilling cores, well logs, seismic and slice identification and analysis, the study region has in sequence developed alluvial fan, braided river, braided river delta, lacustrine facies, as well as the littoral and shallow beaches dam and semi-deep lake turbidite fan. The braided river delta often extends over tens to thousands of square kilometers, and glutenite in subaqueous distributary channel and hydracarbon source rocks frequently deposited with alternative, which constitutes a good source-reserve-seal association in the vertical direction with preferable oil and gas reservoir properties on account of its better rock sorting and the crossrange continuance and connectedness of glutenite. Braided river delta in this region is composed of braided river delta plain subfacies, braided river delta front subfacies and pre-braided river delta subfacies. The plain subfacies is composed of braided channel characterized by various colors, rough granules, poorly graded and erode and stuffed structure existing at the bottom as well as the flood plain formed by migration and flap of the braided channel. What's more, front subfacies chiefly developed all kinds of microfacies, such as distributary channel, mouth bar, distal bar, sand sheet and subaqueous inter-distributary channel.
机译:根据对钻芯,测井,地震和切片识别和分析的分析,研究区域依次开发了冲积扇,辫状河,辫状河三角洲,湖相以及沿岸和浅滩大坝和半坝。深浊浊湖扇。辫状河三角洲通常延伸数万至数千平方公里,水下分流河道中的花岗石和碳氢化合物烃源岩经常被替代沉积,这在垂直方向上构成了良好的储层-储集层结合,并具有较好的油气储层性质。归因于其更好的岩石分选以及方铅矿的跨距连续性和连通性。该地区的辫状河三角洲由辫状河三角洲平原亚相,辫状河三角洲前缘亚相和预辫状河三角洲亚相组成。平原亚相由辫状河道组成,其特征是各种颜色,粗糙的颗粒,不良的坡度和侵蚀以及底部存在的填充结构,以及由辫状河道的迁移和拍打形成的泛滥平原。此外,前亚相主要发育各种微相,如分流河道,河口坝,远侧坝,砂岩和水下水间分流河道。

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