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Fracture development characteristics and controlling factors of Yanchang formation in Heshui area,Ordos Basin |
Xue-Feng QU1, Zhong-Ping ZHAO2( ), Qi-Hong LEI1, Jian LIU1, Wu-Bin GAO1 |
1. Exploration and Development Research Institute,Changqing Oilfield Company,PetroChina,Xi'an 710021,China 2. Beijing Energy Technology Co.,Ltd.,Beijing 100012,China |
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Abstract Based on the comprehensive utilization of drilling data,logging data and 2-D seismic data,the authors hold that the tight reservoir of Yanchang Formation in Heshui area of Ordos Basin has developed a complex fault system consisting of strike-slip faults,fault damage zones and small-scale fractures,which together affect the heterogeneity and flow capacity of underground reservoirs,thus having an important impact on oil and gas production.So faults,fault damage zones and natural small-scale fractures should be treated as a system to analyze the fracture characteristics of ultra-low permeability reservoirs.The authors hold that only considering small-scale fractures is obviously not comprehensive.This understanding has important implications for the study of fractures in ultra-low permeability reservoirs in Ordos Basin.
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Received: 08 July 2019
Published: 22 April 2020
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Corresponding Authors:
Zhong-Ping ZHAO
E-mail: eogt@qq.com
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Schematic location of the study area
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The faults development evidence and distribution map a—fault distribution in development zone;b—2D seismic profile through the W1 well;c—2D seismic profile through the W3 well;d—Chang 6 formation correlation section from well 1 to well 5;e—fault distribution map at Chang 7 formation bottom in Heshui area
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The characteristics of fault damage zone and its distribution in horizontal wells development area a—log curve characteristics of fault damage zone;b—the cores of fault damage zone;c—the overlap map of the drilled fault damage zone in horizontal well development area and the structure map
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Two types of small-scale fractures a—small-scale fractures controlled by lithologic interface;b—small-scale fractures associated with faults
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The relationship between fracture development degree and lithology and bed thickness a—the relationship between fracture development and lithology;b—the histogram of fracture height
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The longitudinal development characteristics of small-scale fractures and its distribution frequency in different zones a—longitudinal distribution of natural fractures in a well;b—statistics on the distribution frequency of small scale fractures at different longitudinal position
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Overlapped map of the fault damage zones distribution and Chang7 bottom structure map in horizontal wells development area(legends are the same as figure3)
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曲率区域 | 水平井 | 直井岩心 | 水平 井数 | 钻遇破 碎带井数 | 破碎带钻遇 井比例/% | 平均破碎 带段数 | 平均破碎 带宽度/m | 裂缝 条数 | 裂缝段岩心 长度/m | 平均每米 裂缝数 | 裂缝段 比例/% | 低曲率区(趋负高值) | 54 | 14 | 25.9 | 2.2 | 2.8 | 107 | 17.45 | 3.82 | 62.321 | 中等曲率区 | 103 | 31 | 30.1 | 3.7 | 4.3 | 230 | 37.07 | 5.35 | 86.209 | 高曲率区(趋正高值) | 102 | 67 | 65.7 | 4.2 | 5.2 | 218 | 31.59 | 4.19 | 60.750 |
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Statistics of small-scale fractures development degree in different curvature area
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