成都理工大学学报(自然科学版)
成都理工大學學報(自然科學版)
성도리공대학학보(자연과학판)
JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY(SCIENCE & TECHNOLOGY EDITION)
2014年
4期
401-412
,共12页
郑荣才%李珂%马启科%李世临%李爽
鄭榮纔%李珂%馬啟科%李世臨%李爽
정영재%리가%마계과%리세림%리상
碳酸盐岩%古喀斯特储层%成岩作用%成岩相%石炭系黄龙组%五百梯气田%四川盆地
碳痠鹽巖%古喀斯特儲層%成巖作用%成巖相%石炭繫黃龍組%五百梯氣田%四川盆地
탄산염암%고객사특저층%성암작용%성암상%석탄계황룡조%오백제기전%사천분지
carbonate rock%karst reservoir%diagenesis%diagenetic facies%Upper Carboniferous Huanglong Formation%Wubaiti gas field%Sichuan Basin
成岩相研究为重要和有效的储层预测技术方法之一。通过钻井岩心描述、薄片鉴定、样品分析,对川东地区五百梯气田石炭系黄龙组碳酸盐岩储层的岩石学、成岩作用、裂缝和储集空间类型等特征进行了综合研究,划分出5种储层成岩相类型,确定以早-中成岩阶段埋藏白云化-晶间孔成岩相为基础,叠加古表生期大气水溶蚀改造的中等溶蚀-孔洞缝成岩相和强溶蚀-角砾成岩相为有利于储层发育的优势成岩相,储集空间主要为粒间和粒内溶孔、晶间溶孔、铸模孔和各种超大溶孔、溶洞和构造裂缝及溶裂缝,认为沉积环境控制了有利储层分布相带、早成岩阶段埋藏白云化奠定了储层发育基础,古表生期喀斯特作用扩大了储层分布范围和发育规模,而破裂作用是提高储层质量的关键。
成巖相研究為重要和有效的儲層預測技術方法之一。通過鑽井巖心描述、薄片鑒定、樣品分析,對川東地區五百梯氣田石炭繫黃龍組碳痠鹽巖儲層的巖石學、成巖作用、裂縫和儲集空間類型等特徵進行瞭綜閤研究,劃分齣5種儲層成巖相類型,確定以早-中成巖階段埋藏白雲化-晶間孔成巖相為基礎,疊加古錶生期大氣水溶蝕改造的中等溶蝕-孔洞縫成巖相和彊溶蝕-角礫成巖相為有利于儲層髮育的優勢成巖相,儲集空間主要為粒間和粒內溶孔、晶間溶孔、鑄模孔和各種超大溶孔、溶洞和構造裂縫及溶裂縫,認為沉積環境控製瞭有利儲層分佈相帶、早成巖階段埋藏白雲化奠定瞭儲層髮育基礎,古錶生期喀斯特作用擴大瞭儲層分佈範圍和髮育規模,而破裂作用是提高儲層質量的關鍵。
성암상연구위중요화유효적저층예측기술방법지일。통과찬정암심묘술、박편감정、양품분석,대천동지구오백제기전석탄계황룡조탄산염암저층적암석학、성암작용、렬봉화저집공간류형등특정진행료종합연구,화분출5충저층성암상류형,학정이조-중성암계단매장백운화-정간공성암상위기출,첩가고표생기대기수용식개조적중등용식-공동봉성암상화강용식-각력성암상위유리우저층발육적우세성암상,저집공간주요위립간화립내용공、정간용공、주모공화각충초대용공、용동화구조렬봉급용렬봉,인위침적배경공제료유리저층분포상대、조성암계단매장백운화전정료저층발육기출,고표생기객사특작용확대료저층분포범위화발육규모,이파렬작용시제고저층질량적관건。
The diagenetic facies analysis is an important and effective method of the reservoir prediction.By drilling core description,thin section identification and sample analysis,the authors make a comprehensive study of the petrology, diagenesis, cracks and spaces of the Upper Carboniferous Huanglong Formation carbonate rock reservoirs in the Wubaiti gas field and determine five kinds of diagenetic facies.They believe that,based on the early to middle burial dolomitization and intergranular pore diagenetic facies,the superimposing medium solution-pores,holes and fracture diagenetic facies and strong dissolution-brecciated diagenetic facies modified by atmospheric water dissolution in the ancient supergene are the predominant facies favorable for the reservoir development.The reservoir spaces are mainly intergranular and intragranular solution pores, intercrystalline solution pores,moldic pores and various oversized solution holes and caves,structural cracks and solution fractures.It is concluded that the depositional environment has controlled the distribution of the favorable reservoirs,the burial dolomitization in the early diagenesis laid a foundation for the reservoir development,the dissolution in the ancient supergene expanded the karst reservoir distribution and developmental scale,and the fracturing is the key to raise the quality of the reservoir.