现代地质
現代地質
현대지질
GEOSCIENCE-JOURNAL OF GRADUATE SCHOOL CHINA UNIVERSITY OF GEOSCIENCES
2014年
3期
626-634
,共9页
冯动军%周洪瑞%肖开华%李秀鹏%王丹丹
馮動軍%週洪瑞%肖開華%李秀鵬%王丹丹
풍동군%주홍서%초개화%리수붕%왕단단
新场地区%须二段%致密砂岩%裂缝%流体
新場地區%鬚二段%緻密砂巖%裂縫%流體
신장지구%수이단%치밀사암%렬봉%류체
Xinchang area%the Second Member of Xujiahe Formation%dense sandstone%fracture%fluids
以川西新场地区须二段致密砂岩储层为研究对象,运用大量薄片资料及物性数据,对储层特征进行分析,利用岩心、测井及地震手段进行裂缝和流体的识别及展布预测,进而达到对储层进行综合评价及优选有利开发区的目的。研究表明须二段次生孔隙及微裂缝发育,裂缝以低角度缝为主,主要沿断层及构造两翼的膝褶带分布。有效储层主要受控于沉积相、成岩、构造及成藏作用,其中溶蚀作用和构造的破裂作用是最重要的控制因素。Ⅰ类储层发育区主要位于上亚段Tx22和中亚段Tx42砂组构造高部位或者大的断裂带附近。结论认为:中、上亚段F3断层两侧为最有利的开发区,其次为上亚段的F1断层南段两侧和中亚段的新10-川科1井区。研究结果可以指导川西新场须二段气藏的有效开发。
以川西新場地區鬚二段緻密砂巖儲層為研究對象,運用大量薄片資料及物性數據,對儲層特徵進行分析,利用巖心、測井及地震手段進行裂縫和流體的識彆及展佈預測,進而達到對儲層進行綜閤評價及優選有利開髮區的目的。研究錶明鬚二段次生孔隙及微裂縫髮育,裂縫以低角度縫為主,主要沿斷層及構造兩翼的膝褶帶分佈。有效儲層主要受控于沉積相、成巖、構造及成藏作用,其中溶蝕作用和構造的破裂作用是最重要的控製因素。Ⅰ類儲層髮育區主要位于上亞段Tx22和中亞段Tx42砂組構造高部位或者大的斷裂帶附近。結論認為:中、上亞段F3斷層兩側為最有利的開髮區,其次為上亞段的F1斷層南段兩側和中亞段的新10-川科1井區。研究結果可以指導川西新場鬚二段氣藏的有效開髮。
이천서신장지구수이단치밀사암저층위연구대상,운용대량박편자료급물성수거,대저층특정진행분석,이용암심、측정급지진수단진행렬봉화류체적식별급전포예측,진이체도대저층진행종합평개급우선유리개발구적목적。연구표명수이단차생공극급미렬봉발육,렬봉이저각도봉위주,주요연단층급구조량익적슬습대분포。유효저층주요수공우침적상、성암、구조급성장작용,기중용식작용화구조적파렬작용시최중요적공제인소。Ⅰ류저층발육구주요위우상아단Tx22화중아단Tx42사조구조고부위혹자대적단렬대부근。결론인위:중、상아단F3단층량측위최유리적개발구,기차위상아단적F1단층남단량측화중아단적신10-천과1정구。연구결과가이지도천서신장수이단기장적유효개발。
In the study of dense sandstone reservoir in the Second Member of Xujiahe Formation in Xinchang area,the reservoir characteristics were analyzed using approved slice and properties data acquired with test methods.Fractures and fluid were identified and predicted using core,logging and seismic methods,to guide the synthetic evaluation of reservoir and the favorable block optimization.It is indicated that secondary pore and micro-fracture develop mostly in target formation,and fractures are mainly low-angle fractures,spreading along fault and fold-belt in structural limbs.The effective reservoir are mainly controlled by sedimentary facies,dia-genesis,structure and petroleum accumulation,however,corrosion and crack are the main control factors.The blocks of reservoirⅠ locate in high structural place or nearby faults in Tx22 and Tx42 .It is concluded that the areas of two sides of F3 fault in middle and up sub-segments are the most favorable blocks,while two sides of southern edge of F1 fault in up sub-segment and Xin10-Chuanke1 well area in middle sub-segment are the sec-ondary.The study results are significant in effective development of the Second Member of Xujiahe Formation in Xinchang area.