四川盆地元坝中部地区须家河组储层裂缝发育特征及控制因素
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范存辉,男,在读博士研究生,从事储层评价、构造地质及裂缝预测等方面的教学与科研工作。联系电话:13438486406,Email: fanchswpi@163.com。

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国家油气重大专项“特低渗透油藏有效开发技术”(2011ZX05013-006),四川省重点学科建设项目“矿产普查与勘探” (SZD0414)。


Characteristics and controlling factors of reservoir fractures in Xujiahe formation, central Yuanba of Sichuan basin
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    摘要:

    四川盆地元坝中部地区须家河组储层属于低孔、低渗透储层,裂缝对其天然气的富集及产量具有重要影响。根据岩心观测、野外露头调查及测井解释等研究成果,综合区域构造演化分析,对元坝中部地区须家河组储层裂缝的发育特征及控制因素进行了系统研究,结果表明,研究区以发育构造成因的低角度剪切裂缝和高角度剪切裂缝为主。裂缝的走向主要为北西西和北东东向,充填程度较低,有效性较好。裂缝的发育受构造应力、构造位置、岩性和岩层厚度等因素控制。随着与断层距离的增大,裂缝密度呈逐渐递减的趋势;中、细砂岩裂缝最为发育,粉砂岩、粗砂岩、砾岩及泥质岩类裂缝发育程度相对较差;随着岩层厚度的增大,裂缝间距变大,发育程度明显降低。研究区裂缝发育区的预测结果表明,裂缝发育区主要位于近南北、北西向展布的大型断裂带附近,主要包括中部元陆1—元陆2井区(不包括元陆2井位置)、元坝5—元陆5—元坝9井区和东部元坝4—花52井区、元陆3井区。

    Abstract:

    The reservoir of Xujiahe formation, lying in the central part Yuanba area, belongs to low porosity-low permeability reservoir,and the fractures in this area have important influence on the accumulation and productivity of gas. Based on the core observation, field investigation and well log interpretation, the development characteristics and controlling factors of fractures are studied systematically,according to the regional tectonic evolution. The results shows that there are tectonic fractures, diagenetic fractures and drilling-induced fractures etc. high-angle shear fractures and low-angle shear fractures caused by tectonic are most developed, which are the key types of factures. The main orientation of fractures lies on NW(290°±10°)and NE(75°±10°). Fractures in this area are poorly filled and are better in petrophysical property. The influencing factors of the fractures development mainly include rock types, rock stratum and the tectonic, etc. The development degree of fractures is different with different lithology; with the increase of layer thickness, the fracture spacing is bigger and the fracture density reduces. The development degree of fractures is sharply decreased. There is a linear relationship between the fracture and he tectonic position. With the distance more and more far away from the faults, the fracture density has a decline trend and the development degree of fractures is also sharply decreased. The comprehensive prediction results of fractures show that the developed zone of fractures is located in both sides of large-scale fault zones, including mainly YL1-YL2(excludingYL2),YB5-YL5-YB9 in the central part of the area and YB4 -H52 and YL3 in the east part of the area.

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范存辉,郭彤楼,王本强,周坤,秦启荣.四川盆地元坝中部地区须家河组储层裂缝发育特征及控制因素[J].油气地质与采收率,2013,20(5):52~54

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  • 在线发布日期: 2015-09-06
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