吉林大学学报(地球科学版)
吉林大學學報(地毬科學版)
길림대학학보(지구과학판)
JOURNAL OF JILIN UNIVERSITY(EARTH SCIENCE EDITION)
2014年
2期
432-445
,共14页
赖锦%王贵文%陈阳阳%黄龙兴%张莉莉%王迪%孙艳慧%李梅
賴錦%王貴文%陳暘暘%黃龍興%張莉莉%王迪%孫豔慧%李梅
뢰금%왕귀문%진양양%황룡흥%장리리%왕적%손염혜%리매
成岩相%川中蓬莱地区%须二段%测井识别方法%优质储集层
成巖相%川中蓬萊地區%鬚二段%測井識彆方法%優質儲集層
성암상%천중봉래지구%수이단%측정식별방법%우질저집층
diagenetic facies%Penglai area in central Sichuan basin%Member 2 of Upper Triassic Xujiahe Formation%logging recognition methods%high quality reservoirs
通过岩心观察并综合利用普通薄片、铸体薄片和扫描电镜分析等资料,对须二段储层岩石学特征、物性及孔隙结构特征、成岩作用、成岩矿物、成岩环境、所处成岩阶段和成岩演化序列等进行了研究。结果表明,须二段储层经历压实压溶、胶结、溶蚀和破裂等成岩作用,现今处于中成岩 A 期。根据成岩作用类型和强度、成岩矿物及其对储层物性的影响划分出3种成岩相:强压实自生矿物胶结相、强压实不稳定组分溶蚀相和破碎裂缝相。选取了对成岩相较敏感的声波时差、电阻率、自然伽马、密度和中子5条常规测井曲线和成像测井资料,通过岩心资料刻度测井建立了各成岩相的测井识别标准,将成岩相进行剖面展开和平面成图。再根据有利成岩相的平面展布规律,对蓬莱地区须二段优质储层发育带进行了预测,认为平面上的斜坡中部为主要的优质储集层发育区。
通過巖心觀察併綜閤利用普通薄片、鑄體薄片和掃描電鏡分析等資料,對鬚二段儲層巖石學特徵、物性及孔隙結構特徵、成巖作用、成巖礦物、成巖環境、所處成巖階段和成巖縯化序列等進行瞭研究。結果錶明,鬚二段儲層經歷壓實壓溶、膠結、溶蝕和破裂等成巖作用,現今處于中成巖 A 期。根據成巖作用類型和彊度、成巖礦物及其對儲層物性的影響劃分齣3種成巖相:彊壓實自生礦物膠結相、彊壓實不穩定組分溶蝕相和破碎裂縫相。選取瞭對成巖相較敏感的聲波時差、電阻率、自然伽馬、密度和中子5條常規測井麯線和成像測井資料,通過巖心資料刻度測井建立瞭各成巖相的測井識彆標準,將成巖相進行剖麵展開和平麵成圖。再根據有利成巖相的平麵展佈規律,對蓬萊地區鬚二段優質儲層髮育帶進行瞭預測,認為平麵上的斜坡中部為主要的優質儲集層髮育區。
통과암심관찰병종합이용보통박편、주체박편화소묘전경분석등자료,대수이단저층암석학특정、물성급공극결구특정、성암작용、성암광물、성암배경、소처성암계단화성암연화서렬등진행료연구。결과표명,수이단저층경력압실압용、효결、용식화파렬등성암작용,현금처우중성암 A 기。근거성암작용류형화강도、성암광물급기대저층물성적영향화분출3충성암상:강압실자생광물효결상、강압실불은정조분용식상화파쇄렬봉상。선취료대성암상교민감적성파시차、전조솔、자연가마、밀도화중자5조상규측정곡선화성상측정자료,통과암심자료각도측정건립료각성암상적측정식별표준,장성암상진행부면전개화평면성도。재근거유리성암상적평면전포규률,대봉래지구수이단우질저층발육대진행료예측,인위평면상적사파중부위주요적우질저집층발육구。
In order to find out distribution zones of high-quality reservoirs in Penglai area,based normal thin sections,casting thin sections,scanning electron microscope analysis data and core data,the reservoirs have been worked on lithological characteristics, reservoir property and pore structure, diagenesis,diagenetic minerals, diagenetic environment, diagenetic stage and diagenetic evolution sequence in Member 2 of Xujiahe Formation.The results show that the reservoirs have experienced diagenesis such as compaction,cementation,corrosion,and fracture,it is now in the stage A of middle diagenetic stage.Three types of diagenetic facies are divided based on diagenesis,diagenetic minerals and their effect on the reservoir quality, these facies include high compaction-authentic minerals cementation facies,high compaction-corrosion of unstable components facies,and tectonic fracture facies.According to various well logging response characteristics,five normal logging curves and imaging logging data which are sensitive to the diagenetic facies are chosen to characterize diagenetic facies,which include compensated neutron logging(CNL),density logging(DEN ),acoustic slowness (AC),natural gamma ray(GR),resistivity log(R t )and EMI,different types of diagenetic facies has various response characteristics on various logging curve and their combination,and the vertical and plane distribution of diagenetic facies can be figured out with well logging data.The favorable diagenetic facies are used to optimize favorable regions of oil and gas bearing zones.The high quality reservoir distributed in the middle part of the slope on the plane surface.