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The structural characteristics and distribution of sand body of the layer 7 of YanChang Formation in Ordos Basin

机译:鄂尔多斯盆地盐昌地区三层砂体的结构特征及分布

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The tight sand in the layer 7 of YanChang Formation, Ordos Basin major develops braided river delta and gravity flow deposits. In this paper, based on previous studies on lake pelvic shape, provenance and hydrodynamic, the sand body in the research area has been systematically studied through core observation, logging data, and sedimentary theory. Various genetic types of sedimentary sand body are developed in this area, mainly as delta deposition, sandy debris flow deposits, turbidites (classic turbidites). We can identify 6 kinds of sand vertical combination type, they are the superimposed sand body(A-type), thick and uniform thickness sand body(B type), thin and uniform thickness sand body (C-type), up thinning sand body (D-type), thickening up sand body (E-type), thick and thin interbed sand body (F-type). The 6 types mainly controlled by sedimentary facies. The A-type sand body mainly developed in the delta depositional environment, the B type sand body is visible both in the delta and slope belt, while the D-type, E-type, F-type sand body are mainly developed in the deep lake. The distribution of sand body in the plane is zonal pattern.
机译:鄂尔多斯盆地主要的延长地层第7层的紧身沙子开发了编织河三角洲和重力流量沉积物。本文基于先前研究湖泊骨质形状,出差和流体动力学的研究,通过核心观察,测井数据和沉积理论系统地研究了研究区域中的砂体。各种遗传类型的沉积砂体是在该领域开发的,主要作为δ沉积,砂岩流量沉积物,浊度(经典浊板)。我们可以识别6种砂垂直组合型,它们是叠加的砂体(A型),厚均匀的厚度砂体(B型),薄而均匀的厚度砂体(C型),稀薄砂体(D型),加厚砂体(E型),厚,薄型砂体(F型)。 6种主要由沉积相控制。 A型砂体主要在三角洲沉积环境中开发,B型砂体在三角洲和斜率带上可见,而D型,E型,F型砂体主要在深处开发湖。飞机中的砂体的分布是区内模式。

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