地质论评
地質論評
지질론평
GEOLOGICAL REVIEW
2015年
1期
163-171
,共9页
赵向原%曾联波%刘忠群%吕文雅%周思宾%刘国平%杜萧笙%李剑
趙嚮原%曾聯波%劉忠群%呂文雅%週思賓%劉國平%杜蕭笙%李劍
조향원%증련파%류충군%려문아%주사빈%류국평%두소생%리검
致密砂岩储层%钙质夹层%天然裂缝%控制作用%天环坳陷
緻密砂巖儲層%鈣質夾層%天然裂縫%控製作用%天環坳陷
치밀사암저층%개질협층%천연렬봉%공제작용%천배요함
tight sandstone reservoir%calcareous interbeds%natural fracture%controlling effect%Tianhuan depression
鄂尔多斯盆地镇泾区块长8致密砂岩储层普遍发育钙质夹层,本文利用露头、岩芯、薄片及测井等资料,对钙质夹层的岩性特征、电性特征、分布规律以及与天然裂缝分布的关系进行了研究。研究表明,钙质夹层具有明显的低伽马、低声波时差、高密度、高感应的特点,电成像测井表现为明显的亮色条带。钙质夹层主要分布在部分水下分流河道砂体的中部或下部及河口坝砂体的中部或上部,同时也发育在一些分选较好、颗粒支撑的薄层细砂岩中以及砂泥岩的接触地带。钙质夹层内主要发育高角度构造裂缝,不发育近水平成岩裂缝;与非钙质胶结致密砂岩储层相比,钙质夹层脆性较大,天然裂缝更为发育,且大部分裂缝被方解石充填,为无效裂缝;钙质夹层层厚及岩性界面控制着裂缝纵向延伸高度。论文成果对进一步研究致密储层天然裂缝的分布模式,弄清裂缝对注水开发的影响具有重要意义。
鄂爾多斯盆地鎮涇區塊長8緻密砂巖儲層普遍髮育鈣質夾層,本文利用露頭、巖芯、薄片及測井等資料,對鈣質夾層的巖性特徵、電性特徵、分佈規律以及與天然裂縫分佈的關繫進行瞭研究。研究錶明,鈣質夾層具有明顯的低伽馬、低聲波時差、高密度、高感應的特點,電成像測井錶現為明顯的亮色條帶。鈣質夾層主要分佈在部分水下分流河道砂體的中部或下部及河口壩砂體的中部或上部,同時也髮育在一些分選較好、顆粒支撐的薄層細砂巖中以及砂泥巖的接觸地帶。鈣質夾層內主要髮育高角度構造裂縫,不髮育近水平成巖裂縫;與非鈣質膠結緻密砂巖儲層相比,鈣質夾層脆性較大,天然裂縫更為髮育,且大部分裂縫被方解石充填,為無效裂縫;鈣質夾層層厚及巖性界麵控製著裂縫縱嚮延伸高度。論文成果對進一步研究緻密儲層天然裂縫的分佈模式,弄清裂縫對註水開髮的影響具有重要意義。
악이다사분지진경구괴장8치밀사암저층보편발육개질협층,본문이용로두、암심、박편급측정등자료,대개질협층적암성특정、전성특정、분포규률이급여천연렬봉분포적관계진행료연구。연구표명,개질협층구유명현적저가마、저성파시차、고밀도、고감응적특점,전성상측정표현위명현적량색조대。개질협층주요분포재부분수하분류하도사체적중부혹하부급하구패사체적중부혹상부,동시야발육재일사분선교호、과립지탱적박층세사암중이급사니암적접촉지대。개질협층내주요발육고각도구조렬봉,불발육근수평성암렬봉;여비개질효결치밀사암저층상비,개질협층취성교대,천연렬봉경위발육,차대부분렬봉피방해석충전,위무효렬봉;개질협층층후급암성계면공제착렬봉종향연신고도。논문성과대진일보연구치밀저층천연렬봉적분포모식,롱청렬봉대주수개발적영향구유중요의의。
Calcareous interbeds develop widely in Chang 8 tight sandstone reservoirs,Zhenjing Area,Ordos Basin.This paper reported the lithology,electricity,distributing characteristies of the calcareous interbed and the relationship with the distribution of natural fractures based on outcrops,cores and logs data.Studies have shown that calcareous interbeds have the following electrical characteristics.Natural gamma ray log is low.Longitudinal wave offset and transverse wave offset time are also low.The value of density logging is high and induction logging is obvious high.Electric imaging logging has the characteristic of clear light yellow (light).Good development of calcareous interbeds presents at the middle or bottom of underwater distributary channel sand body and at the top or middle of mouth bar sand body in delta front.Besides,calcareous interbeds are distributed in well-sorted,grain supported fine sandstones and contact zones of mudstones and sandstones.There are mainly high angle tectonic fractures in calcareous interbeds with little nearly horizontal diagenetic fractures.Calcareous interbeds are brittler than non-calcareous cementation tight sandstone.In consequence there are more natural fractures and the majority of them are filled with calcite taken as invalid.The thickness and lithologic interface of calcareous inerbeds determine the longitudinal height of fractures.All the achievements of this thesis are significant to study the distribution patterns of natural fractures and the effect of fractures on water flooding development.