复杂油气藏
複雜油氣藏
복잡유기장
COMPLEX HYDROCARBON RESERVOIRS
2012年
1期
1-4
,共4页
王时林%秦启荣%黄亮%樊佐春
王時林%秦啟榮%黃亮%樊佐春
왕시림%진계영%황량%번좌춘
裂缝%裂缝特征%控制因素%营城组%十屋油田
裂縫%裂縫特徵%控製因素%營城組%十屋油田
렬봉%렬봉특정%공제인소%영성조%십옥유전
fracture%fracture characteristics%control factors%Yingcheng Formation%Shiwu Oilfield
十屋油田营城组属于低孔、特低渗储层,裂缝能最有效地提高储层渗透率。通过岩心裂缝描述,镜下观察,对十屋油田营城组低孔、特低渗储层构造裂缝的组系和产状、裂缝长度、宽度、密度、充填特征、期次及其主要控制因素进行了分析研究。结果表明,十屋油田营城组主要发育四期裂缝,分别为营城末期和登娄库末期发育的近南北( 10°± 15°) 向和近东西( 290°±15°) 向的高角度共轭剪切缝、北东( 45°±15°) 向控盆断裂的伴生缝、北西( 325°±15°) 向高角度张性缝、嫩江末期和明水末期发育的北东向( 45°±15°) 派生剪切缝和北北东( 35°±15°) 向及北西( 325°±15°) 向的高角度直立剪切裂缝。裂缝发育分布主要受控于岩性、构造应力场和构造位置。通过对十屋油田营城组裂缝的研究,为十屋油田营城组勘探开发提供了方向和依据。
十屋油田營城組屬于低孔、特低滲儲層,裂縫能最有效地提高儲層滲透率。通過巖心裂縫描述,鏡下觀察,對十屋油田營城組低孔、特低滲儲層構造裂縫的組繫和產狀、裂縫長度、寬度、密度、充填特徵、期次及其主要控製因素進行瞭分析研究。結果錶明,十屋油田營城組主要髮育四期裂縫,分彆為營城末期和登婁庫末期髮育的近南北( 10°± 15°) 嚮和近東西( 290°±15°) 嚮的高角度共軛剪切縫、北東( 45°±15°) 嚮控盆斷裂的伴生縫、北西( 325°±15°) 嚮高角度張性縫、嫩江末期和明水末期髮育的北東嚮( 45°±15°) 派生剪切縫和北北東( 35°±15°) 嚮及北西( 325°±15°) 嚮的高角度直立剪切裂縫。裂縫髮育分佈主要受控于巖性、構造應力場和構造位置。通過對十屋油田營城組裂縫的研究,為十屋油田營城組勘探開髮提供瞭方嚮和依據。
십옥유전영성조속우저공、특저삼저층,렬봉능최유효지제고저층삼투솔。통과암심렬봉묘술,경하관찰,대십옥유전영성조저공、특저삼저층구조렬봉적조계화산상、렬봉장도、관도、밀도、충전특정、기차급기주요공제인소진행료분석연구。결과표명,십옥유전영성조주요발육사기렬봉,분별위영성말기화등루고말기발육적근남북( 10°± 15°) 향화근동서( 290°±15°) 향적고각도공액전절봉、북동( 45°±15°) 향공분단렬적반생봉、북서( 325°±15°) 향고각도장성봉、눈강말기화명수말기발육적북동향( 45°±15°) 파생전절봉화북북동( 35°±15°) 향급북서( 325°±15°) 향적고각도직립전절렬봉。렬봉발육분포주요수공우암성、구조응력장화구조위치。통과대십옥유전영성조렬봉적연구,위십옥유전영성조감탐개발제공료방향화의거。
The Yingcheng Formation of Shiwu Oilfield belongs to a low porosity and ultra-low permeability reservoir,and fractures in the formation can effectively increase reservoir permeability.The systems and altitude,length,width,density,and controlling factors of the fractures were investigated by using data of core description.The fractures of the Yingcheng Formation,which were mainly developed through four periods,consist of high angle conjugated shear fractures in nearly south-north direction and nearly east -west direction,associated fractures of basin-controlling-fault in north-east direction,and high angle tension fractures in north-west direction in the end of Yingcheng and Denglouku stage,and derived shear fractures in north-east direction and high angle up-right shear factures in north-east and north-west direction in the end of Nenjiang and Mingshui stage.The development and distribution of the fractures were controlled by lithologic characteristics,regional tectonic stress,and tectonic position.