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威远地区龙马溪组天然裂缝特征、分布规律及形成期次

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为了深入研究四川盆地非常规油气勘探开发的关键层位,以川南威远地区龙马溪组天然裂缝为研究对象,通过岩心观察、薄片分析和地球化学测试等多种方法分析了该区龙马溪组天然裂缝发育特征和形成时期,指出了该区龙马溪组天然裂缝发育类型及其形成期次.研究结果表明:①威远地区天然裂缝主要分为构造裂缝、生烃超压缝和层理缝3种类型;②威远龙马溪组存在多期天然裂缝.结论认为:①该区天然裂缝具有宽度细、水平层理缝占比高、偶见高角度构造缝、有效性低的特点,并且随着龙马溪组地层埋深的增加,裂缝发育密度逐渐增大;②根据温度计算和构造埋藏演化史,这些天然裂缝主要形成于印支期、燕山期、喜马拉雅晚期的3个时期,其中碳氧同位素和包裹体实验测试证实了3个时期的天然裂缝存在;③研究区印支期发育少量的NW剪切缝及砂泥互层层理缝,燕山期在断层附近、背斜高部位发育NW剪切缝和生烃超压缝,喜马拉雅晚期在断层附近、背斜高部位发育近NW和NWW组系剪切缝,背斜核部发育近S-N组系张性缝.结合研究区地质力学环境,查明了威远地区龙马溪组天然裂缝特征,明确了裂缝的形成期次及分布规律,为威远龙马溪组储层评价、有利区优选、优质储层甜点区评价及勘探开发提供了技术支撑.
Natural fractures in the Longmaxi Formation,Weiyuan block:Characteristics,distribution patterns and forming episodes
To comprehend the major interesting reservoirs for both exploration and development of unconventional oil and gas in Sichuan Basin,natural fractures in the Longmaxi Formation,Weiyuan block,southern Sichuan Basin,were taken as objectives.Their development characteristics and forming timing were analyzed by means of core observation,thin-section identification and geochemical experiments.Additionally,both development types and forming episodes were defined.Re-sults show that(ⅰ)these fractures can be mainly classified into three types of structural fracture,hydrocarbon-generating overpressured fracture and bedding fracture;and(ⅱ)there exist multi-episode fractures in this formation.Three conclu-sions have been made.First,Weiyuan area often witnesses natural fractures with smaller width and high proportion of hori-zontal-bedding fractures while occasionally high-angle structural ones with low effectiveness.Moreover,the density of frac-ture extension increases gradually with the increasing burial depth of the Longmaxi Formation.Second,based on tempera-ture calculation and structural depth evolution,it is demonstrated that these fractures were dominantly formed in the Indo-sinian,Yanshanian and late Himalayanian epochs.And carbon/oxygen isotope and inclusion experiments all confirm their existence in these three epochs.Third,in the study area,it can be found a small number of NW-strike shear fractures and bedding fractures of sandstone interbedded with mudstone developed in the Indosinian epoch,NW-trending shear and hy-drocarbon-generating overpressured fractures near faults or at anticline high in the Yanshanian epoch,nearly NW-and NWW-strike shear fractures also close to faults or at anticline high in the late Himalayanian epoch,and nearly S-N-strike tensile fractures developed at anticlinal core in the late Himalayanian epoch,respectively.Finally,based on the geome-chanical setting of Weiyuan block,the characteristics,forming episodes and distribution patterns have been figured out for these natural fractures,which may provide technical support for the reservoir evaluation,favorable selection,sweetspot as-sessment together with exploitation of the Longmaxi Formation in this block.

Sichuan BasinWeiyuan blockLower Silurian Longmaxi FormationNatural fractureDistribution characteris-ticsStage evolution

郝越翔、刘佳杰、吴磊、周昕、李洁辛、江雨濛

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中国石油川庆钻探工程有限公司页岩气勘探开发项目经理部,四川 成都 610051

成都理工大学地球物理学院,四川 成都 610059

四川盆地 威远地区 下志留统龙马溪组 天然裂缝 分布特征 期次演化

2024

天然气技术与经济
中国石油西南油气田公司

天然气技术与经济

影响因子:0.459
ISSN:2095-1132
年,卷(期):2024.18(1)
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