岩性油气藏
巖性油氣藏
암성유기장
LITHOLOGIC RESERVOIRS
2012年
2期
21-25
,共5页
陈吉%张永梅%史基安%张永庶%孙国强%王国仓
陳吉%張永梅%史基安%張永庶%孫國彊%王國倉
진길%장영매%사기안%장영서%손국강%왕국창
成岩作用%原生孔隙%储层物性%柴北缘
成巖作用%原生孔隙%儲層物性%柴北緣
성암작용%원생공극%저층물성%시북연
diagenesis%primary pore%reservoir properties%northern Qaidam Basin
运用岩心、铸体薄片、扫描电镜和化验资料等,系统研究了柴达木盆地北缘冷湖—马仙地区古近系—新近系成岩作用特征及其对储层物性的影响。研究表明,柴北缘冷湖—马仙地区古近系—新近系储集砂岩主要为岩屑长石砂岩、长石砂岩和长石岩屑砂岩。主要成岩作用为压实作用、胶结作用和溶蚀作用。压实作用以机械压实为主;胶结作用主要为碳酸盐胶结、硫酸盐胶结、石英次生加大和黏土矿物胶结;溶蚀作用主要为碳酸盐岩和碎屑颗粒的溶蚀。压实作用和胶结作用是原生孔隙减少以及储层物性变差的主要原因。碎屑颗粒和胶结物的溶蚀是次生孔隙形成的主要原因。
運用巖心、鑄體薄片、掃描電鏡和化驗資料等,繫統研究瞭柴達木盆地北緣冷湖—馬仙地區古近繫—新近繫成巖作用特徵及其對儲層物性的影響。研究錶明,柴北緣冷湖—馬仙地區古近繫—新近繫儲集砂巖主要為巖屑長石砂巖、長石砂巖和長石巖屑砂巖。主要成巖作用為壓實作用、膠結作用和溶蝕作用。壓實作用以機械壓實為主;膠結作用主要為碳痠鹽膠結、硫痠鹽膠結、石英次生加大和黏土礦物膠結;溶蝕作用主要為碳痠鹽巖和碎屑顆粒的溶蝕。壓實作用和膠結作用是原生孔隙減少以及儲層物性變差的主要原因。碎屑顆粒和膠結物的溶蝕是次生孔隙形成的主要原因。
운용암심、주체박편、소묘전경화화험자료등,계통연구료시체목분지북연랭호—마선지구고근계—신근계성암작용특정급기대저층물성적영향。연구표명,시북연랭호—마선지구고근계—신근계저집사암주요위암설장석사암、장석사암화장석암설사암。주요성암작용위압실작용、효결작용화용식작용。압실작용이궤계압실위주;효결작용주요위탄산염효결、류산염효결、석영차생가대화점토광물효결;용식작용주요위탄산염암화쇄설과립적용식。압실작용화효결작용시원생공극감소이급저층물성변차적주요원인。쇄설과립화효결물적용식시차생공극형성적주요원인。
Based on cores,cast thin sections,scanning electron microscope and testing data,this paper studied the diagenesis of Paleogene-Neogene sandstone reservoirs and its influence on reservoir properties in Lenghu-Maxian area in north Qaidam Basin.The result shows that the sandstone reservoirs in this area are mainly composed of lithic arkose,arkose and feldspar lithic sandstone,and mainly experienced such actions as compaction,cementation and dissolution.Mechanical compaction is the main compaction,cementations are mainly carbonate cementation,sulfate cementation,quartz overgrowth and clay minerals cementation,and dissolution comprises carbonate cementation content and detrital dissolution.Compaction and cementation caused the destruction of primary pores and made the reservoir properties poor.Dissolution of the lithic and cement was the main reason for generating secondary pores.According to the characteristics of vitrinite reflectance and clay minerals,it is ascertained that the evolution have reached the early diagenetic stage A,and the minor part reached the middle diagenetic stage B.