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Distribution of shallow water delta sand bodies and the genesis of thick layer sand bodies of the Triassic Yanchang Formation, Longdong Area, Ordos Basin

机译:鄂尔多斯盆地三叠纪盐昌地区浅层三角洲砂体的分布及厚层砂体的成因

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摘要

Based on the cores from 47 wells and logging data of 130 wells,the main types of sand bodies in the shallow water delta of the Chang 8_(2) sub-member in the Triassic Yanchang Formation,Longdong Area,Ordos Basin were comprehensively analyzed,the distribution characteristics of sand bodies more than 20 m thick were identified,and the genetic types of the thick sand bodies were sorted out.In this region,thick-bed sand bodies can be divided into two types according to the shape and position:type 1 is the sand body in wide strip and is distributed between the average high water mark and the average low water mark;type 2 is distributed on both sides of the average low water mark and is in irregular lump shape.Based on the principle of the volume distribution of sediments and the change rule of accommodation space,the genetic models of two types of thick-bed sand bodies in the Chang 8_(2) sub-member are superimposed distributary channel sand bodies in high accommodation space and superimposed composite sand bodies in low accommodation space.
机译:基于来自47孔的核心和130孔的测井数据,鄂尔多斯盆地三叠纪盐昌地区昌8_(2)个子成员的浅水三角洲的主要类型的砂体进行了全面分析,鉴定了超过20米厚的砂体的分布特性,并将厚砂体的遗传类型分开。在该区域,厚床砂体可根据形状和位置分为两种类型:型1是宽带的砂体,分布在平均高水标记和平均低水标记之间; 2型分布在平均低水标记的两侧,并且处于不规则的块状。基于原理沉积物的体积分布和容纳空间的变化规则,在高8_(2)个子构件中两种厚床砂体的遗传模型是高容纳空间的叠加分布通道砂体和叠加复合砂体在低住宿空间。

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