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现代地质 ›› 2018, Vol. 32 ›› Issue (06): 1182-1193.DOI: 10.19657/j.geoscience.1000-8527.2018.06.07

• 石油地质学 • 上一篇    下一篇

低渗透储层不同成岩相微观孔隙结构特征及其测井识别差异性分析:以姬塬油田王盘山长61储层为例

韩进1,2(), 孙卫1, 杨波3, 樊秀江4, 吴彦君5   

  1. 1.西北大学 大陆动力学国家重点实验室/地质学系,陕西 西安 710069
    2.延安大学 石油工程与环境工程学院,陕西 延安 716000
    3.陕西省煤层气开发利用有限公司,陕西 西安 710075
    4.延长油田股份有限公司 七里村采油厂,陕西 延安 716000
    5.延长油田股份有限公司 宝塔采油厂,陕西 延安 716000
  • 收稿日期:2018-01-20 修回日期:2018-06-17 出版日期:2018-12-10 发布日期:2018-12-20
  • 作者简介:韩 进,男,博士研究生,讲师,1983年出生,油气田地质与开发专业,主要从事采油采气工程理论与技术研究工作。Email:380497965@qq.com
  • 基金资助:
    陕西省教育厅专项科研计划项目(15JK1812);延安大学自然科学专项基金项目(YDQ2013-23)

Characteristics of Micro-pore Structure and Differential Analysis of Logging Identification for Different Diagenetic Facies in Low Permeability Reservoir:A Case Study on Chang 61 Reservoir in Wangpanshan Area of Jiyuan Oilfield

HAN Jin1,2(), SUN Wei1, YANG Bo3, FAN Xiujiang4, WU Yanjun5   

  1. 1. State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi’an,Shaanxi 710069, China
    2. College of Petroleum Engineering and Environmental Engineering, Yan’an University, Yan’an, Shaanxi 716000, China
    3. Shaanxi Coalbed Methane Development Co.Ltd., Xi’an, Shaanxi 710075,China
    4. Qilicun Oil Production Plant of Yanchang Oilfield, Yan’an, Shaanxi 716000, China
    5. Baota Oil Production Plant of Yanchang Oilfield, Yan’an, Shaanxi 716000, China
  • Received:2018-01-20 Revised:2018-06-17 Online:2018-12-10 Published:2018-12-20

摘要:

基于铸体薄片、扫描电镜、岩心照片、恒速压汞等资料,综合考虑物源、黏土矿物类型、孔隙类型、成岩作用等参数将王盘山长61储层划分成6种不同组合类型成岩相,其中优势储集成岩相为高岭石+绿泥石胶结-粒间孔相、高岭石胶结-溶孔+粒间孔相、绿泥石+高岭石胶结-溶孔相等。研究表明:不同类型成岩相的微观孔隙结构特征及测井响应特征不同,各成岩相微观孔喉差异明显,尤其体现在毛管压力曲线和喉道上,喉道半径与渗透率的相关性好于孔隙半径与孔隙度、渗透率的相关性,优势成岩相孔喉半径较均匀、连通性好、渗流能力较强,相同进汞压力条件下进汞饱和度高;利用自然伽马、声波时差、电阻率等测井曲线,归纳了不同成岩相的测井响应特征,建立了各成岩相测井响应识别模板,确定了不同成岩相的测井响应定量判别标准,最终实现储层纵向上成岩相的识别与划分,为低渗透砂岩储层甜点预测提供重要参考。

关键词: 长61储层, 成岩相, 恒速压汞, 喉道, 测井曲线

Abstract:

Based on information from casting thin sections, scanning electron microscopy (SEM), core photos and constant speed mercury pressure analysis, and with the consideration of the material source, clay mineral, pore type and diagenesis, the Chang 61 reservoir of Wangpanshan is divided into six different diagenetic facies. The dominant reservoir facies are kaolinite+chlorite cementation-intergranular pore, kaolinite cementation-dissolved pore+intergranular pore, and chlorite+kaolinite cementation-dissolution pore. This study shows that the microscopic pore structures and logging responses of the different diagenetic facies are various. The variation of micro-pore throat in each diagenetic phase is distinct, especially in the capillary pressure curve and throat. Correlation between the throat radius and permeability is better than that between the pore radius, porosity and permeability. Moreover, the pore throat radius of the dominating diagenetic facies is more uniform, with better connectivity and seepage ability, which keep high mercury saturation under the same pressure of the mercury intake. The logging response characteristics of the different diagenetic facies are summed up by using natural gamma ray, sonic time difference, resistivity and other logging curves. We then established the logging response identification template for each diagenetic facies, and determined the quantitative identification criteria for logging response of the different diagenetic facies. With that, we identified and divided the vertical upper diagenetic facies of the single well, which provide an important reference for the prediction of sweet spot in low permeability sandstone reservoirs.

Key words: Chang 61 reservoir, diagenetic facies, constant speed mercury penetration, throat, logging curve

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