Fractured Zone Detection Using Petrophysical Logs by Rescaled Windowed R/S Analyses and Discrete Fracture Network (DFN) of Yanchang Formation in Mahuangshan-Hongliugou Area, Ordos Basin, China

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2023-09-28 DOI:10.1155/2023/9255499
Jindong Gao, Lirong Li, Gaorun Gao, Shuwei Ma, Meng Li
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引用次数: 0

Abstract

Structural fractures generally develop in the upper crust strata and are usually distributed in a convergent pattern, forming structural fracture zones with a specific strike. Fracture zones control the reservoir seepage system and seriously affect the migration and accumulation of oil and gas in tight sandstone reservoirs. Therefore, characterizing the characteristics of the fracture zones for tight oil exploration and development effectively is essential. In this paper, the variable scale fractal method is introduced to calculate the petrophysical log, and a new curve H is built. An intensity log is to characterize the intensity of structural fracture development. The H curve is in a good linear relationship with the intensity curve after the comparison of the H curve and intensity curve in 32 wells. A quantitative relationship between H and the intensity curve is established. Based on the parameters obtained from the core and image logs, the discrete fracture network model was established using H curves from more than 300 wells, and the structural fracture zone was analyzed. The model shows that the fracture zones formed by structural fractures are in S-N and NW-SE directions in the study area. The orientation of the structural fracture zone is consistent with that of the fractured fault zone and fault, and the development of the fractured zone is consistent with the regional tectonic evolution characteristics. The characteristics of the fracture zone explain the distribution law of oil accumulation and groundwater salinity in the study area.
鄂尔多斯盆地马黄山—红柳沟地区延长组岩石物理测井裂缝带重标窗R/S分析及离散裂缝网络探测
构造裂缝一般发育在上地壳地层中,通常呈会聚型分布,形成特定走向的构造断裂带。裂缝带控制着储层渗流系统,严重影响致密砂岩储层油气的运移和聚集。因此,有效表征裂缝带特征对致密油勘探开发至关重要。本文引入变尺度分形法计算岩石物理测井曲线,建立了一条新的曲线H。强度测井用来描述构造裂缝发育的强度。对比32口井的H曲线和强度曲线,发现H曲线与强度曲线呈良好的线性关系。建立了H与强度曲线之间的定量关系。根据岩心参数和图像测井资料,利用300多口井的H曲线建立离散裂缝网络模型,并对构造裂缝带进行分析。模型显示,研究区构造裂缝形成的裂缝带主要分布在南北向和北西-东南向。构造断裂带的走向与断裂断裂带和断裂的走向一致,断裂带的发育与区域构造演化特征一致。裂缝带的特征解释了研究区油气聚集和地下水盐度的分布规律。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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