油气藏评价与开发

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塔里木盆地迪那2气藏构造裂缝特征与水侵规律研究

毛金昕1,解馨慧2,邓虎成1,王志民3,李朋1,吴永平3,相泽厚1,张鑫2   

  1. 1.成都理工大学能源学院,四川 成都 610059;
    2.成都理工大学地球物理学院,四川 成都 610059;
    3.中国石油塔里木油田分公司勘探开发研究院,新疆 库尔勒 841000

Research on tectonic fracture characteristics and water invasion dynamics of the Dina-2 gas reservoir in the Tarim Basin

MAO Jinxin1(), XIE Xinhui2, DENG Hucheng1(), WANG Zhimin3, LI Peng1, WU Yongping3, XIANG Zehou1, ZHANG Xin2   

  1. 1. College of Energy, Chengdu University of Technology, Chengdu, Sichuan 610059, China;
    2. College of Geophysics, Chengdu University of Technology, Chengdu, Sichuan 610059, China;
    3. Research Institute of Exploration and Development of PetroChina Tarim Oilfield Branch Company, Korla, Xinjiang 841000, China

摘要:

迪那2气藏为塔里木盆地一大型边水致密砂岩气藏,储层非均质性强,天然裂缝是影响其高产和水侵的重要因素。裂缝研究对明确气藏水侵规律及防控水政策的制定意义重大。研究基于岩心、薄片、成像测井等地质资料,分析天然裂缝地质静态特征。结合产水、产气、压力等生产动态特征,分析不同因素对水侵的影响,利用层次分析法明确控制因素,研究不同形态构造裂缝对水侵特征影响,建立气藏水侵模式。研究结果表明:研究区构造裂缝分为剪切裂缝和张性裂缝,以充填裂缝为主,充填物主要为方解石,其次是石英和黏土等,但开度较大;根据生产动态特征可以分为早期暴性水淹井、晚期暴性水淹井、带水生产井和无水生产井,4种类型生产井生产特征明显不同;依据生产特征和地质特征,从构造位置、断层、隔层、地层系数和裂缝5个因素对研究区气藏主控因素分析,明确裂缝为主要因素,断层、隔层、地层系数为次要因素,构造位置为无关因素,利用层次分析法建立水侵综合评价指数;结合裂缝形态差异及生产特征,明确了复杂裂缝对气井高产及产水的影响。以此建立了优势裂缝型、断缝体局限型和优势裂缝-断层-砂体组合型的3种水侵模式,总结气藏水侵规律。研究成果对类似气藏开发具有一定的指导意义,为同类型有水气藏水侵规律研究和开发评价提供借鉴。

关键词: 塔里木盆地, 库车坳陷, 天然裂缝, 水侵特征, 水侵模式

Abstract:

The Dina-2 Gas Reservoir, a large-scale edge-water tight sandstone gas reservoir in the Tarim Basin, exhibits strong reservoir heterogeneity, with natural fractures critically governing its high productivity and water invasion dynamics. Fracture characterization is pivotal for deciphering water invasion mechanisms and optimizing water control strategies. This study integrates geological data including core samples, thin-section analysis, and image logging to evaluate the static geological attributes of natural fractures, while production dynamics such as water and gas rates and pressure data are analyzed to assess multi-factor impacts on water influx. By applying the Analytic Hierarchy Process, controlling factors are systematically prioritized, revealing that tectonic fracture morphologies, classified as shear fractures and tensile fractures predominantly filled with calcite followed by quartz and clay minerals yet displaying significant apertures,dominate water invasion behaviors. Production wells are categorized into four distinct types based on dynamic performance: early-stage violent water-flooded wells, late-stage violent water-flooded wells, water-producing wells, and water-free wells, each exhibiting unique production trends. Integrated evaluation of structural position, faults, interlayers, matrix properties, and fractures identifies fractures as theprimary controlling factor, with faults, interlayers, and matrix acting as secondary contributors, while structural position shows negligible influence. A comprehensive water invasion evaluation index is established via the Analytic Hierarchy Process, underscoring the dual role of complex fracture networks in enhancing gas productivity and exacerbating water breakthrough risks. Three water invasion patterns are proposed: dominant fracture-controlled, fault-fracture compartment-controlled, and fault-dominant fracture-sandbody composite types,collectively delineating the reservoir's water invasion mechanisms. These findings offer strategic guidance for developing analogous heterogeneous fractured tight sandstone gas reservoirs and provide critical insights for water invasion mechanism research and development evaluation in similar water-bearing gas reservoirs.

Key words: Tarim Basin, Kuqa depression, natural fractures, water invasion characteristic, water intrusion pattern