断层砂岩储层中的断裂

Shuai Yin , Yuanyuan Lu , Junhui Zhao
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引用次数: 0

摘要

鄂尔多斯盆地西南部延长地层长8系是典型的断层砂岩油藏。裂缝的发育特征对致密油藏甜点的形成具有明显的控制作用。本文以鄂尔多斯盆地西南部的长8系为例,系统研究了断层砂岩油藏裂缝发育特征及控制因素。结果表明,研究区内的断层砂岩油藏沿主要走向-滑动断层分布。断裂系统包括垂直断裂和水平层理断裂。垂直断裂的断裂面一般具有较好的出油性,多表现为油斑和油浸层;而水平埋藏断裂的出油性一般表现为油斑层。水平层理裂缝的发育频率为 62.5%,垂直裂缝的发育频率为 37.5%。裂缝主要发育在细砂岩中,少量发育在中粒砂岩和粉砂岩中。影响断层油藏裂缝发育程度的因素包括距主断层的距离、砂层厚度、岩性和构造位置。在泾河油田和红河油田,当与主断层的距离分别大于 1.25 千米和 1.5 千米时,断裂发育程度急剧下降。单砂体厚度也控制着断裂发育程度。河槽翼部砂体较薄,粒度较细,压实空间小,在构造活动作用下易断裂。研究区内长8系断裂主要发育在断层、反斜顶部及其翼部附近。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Fractures in faulted sandstone reservoir

Fractures in faulted sandstone reservoir

The Chang 8 Member of the Yanchang Formation in southwest Ordos Basin is a typical faulted sandstone oil reservoir. The development characteristics of fractures have obvious controlling effect on the formation of sweet spots of tight reservoir. In this paper, taking the Chang 8 Member of the southwestern Ordos Basin as an example, the development characteristics and controlling factors of fractures in faulted sandstone oil reservoir are systematically studied. The results show that the faulted sandstone oil reservoirs in the study area are distributed along the main strike-slip faults. The fracture system includes vertical fractures and horizontal bedding fractures. The fracture surface of vertical fractures generally has good oil display, and mostly presented as oil spot and oil immersion level; however, the oil level of horizontal bedding fractures is usually presented as oil spot level. The development frequency of horizontal bedding fractures is 62.5 %, while that of vertical fractures is 37.5 %. The fractures are mainly developed in fine sandstone and a small amount of medium-grained sandstone and siltstone. The factors that affect the fracture development degree in faulted oil reservoir include the distance from main fault, sand thickness, lithology and structural location. For the Jinghe and Honghe Oilfields, the degree of fracture development decreases sharply when the distance from the main fault is greater than 1.25 km and 1.5 km, respectively. Single sand body thickness also controls the degree of fracture development. Single sand bodies with thickness within 6 m have more developed fractures, and the fracture development decreases sharply when the thickness exceeds 6 m. The sand body in the wing part of river channel is relatively thin with fine grain size and small compacted space, which is easy to break under tectonic activity. The fractures of the Chang 8 Member in the study area are mainly developed near the faults, the top of anticline and its wing part.

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