石油与天然气地质 ›› 2022, Vol. 43 ›› Issue (4): 902-916.doi: 10.11743/ogg20220413
刘自亮1,2(), 张明何1,2(), 刘四兵1,2, 王均杰3, 郝景宇3, 陈义才1,2, 周月1,2
收稿日期:
2022-03-22
修回日期:
2022-05-05
出版日期:
2022-07-14
发布日期:
2022-07-14
通讯作者:
张明何
E-mail:bugliu2001@163.com;1102553662@qq.com
作者简介:
刘自亮(1978—),男,博士、副教授,沉积学、储层地质学。E?mail: 基金资助:
Ziliang Liu1,2(), Minghe Zhang1,2(), Sibing Liu1,2, Junjie Wang3, Jingyu Hao3, Yicai Chen1,2, Yue Zhou1,2
Received:
2022-03-22
Revised:
2022-05-05
Online:
2022-07-14
Published:
2022-07-14
Contact:
Minghe Zhang
E-mail:bugliu2001@163.com;1102553662@qq.com
摘要:
广西雪峰山南缘石炭系寺门组具有较好的油气成藏背景条件,查明寺门组储层的形成发育机制及其控制因素对该区油气勘探具有重要意义。利用野外露头、钻井和岩心资料,结合运用扫描电镜、铸体薄片、包裹体和孔-渗分析等手段,明确了广西雪峰山南缘石炭系寺门组储层的基本特征,探讨了储层发育的控制因素及优质储层形成模式和有利区分布。研究表明,寺门组储层岩石类型主要为细粒石英砂岩和岩屑质石英砂岩;储集空间包括原生粒间孔、次生溶蚀孔和裂缝;储层类型属于孔隙-裂缝型和孔隙型,整体呈低孔、低渗特征。储层质量主要受沉积、成岩及构造作用的共同控制:沿岸砂坝、砂泥质滨岸和混合坪微相控制了寺门组储层砂体的分布;强烈的压实作用是储层致密化的最主要原因,造成的孔隙损失率约85.2 %;溶蚀作用使储层质量得到有效提升(增孔量约2.3 %);构造裂缝极大地促进了储层的输导能力,使局部地区仍具备优质储层发育的物性条件。最后,建立了储层发育模式,预测研究区存在德胜和洛埠2个有利储层分布区。
中图分类号:
图4
雪峰山南缘寺门组储层储集空间类型及特征a.粒间孔(红色箭头)和粒间溶孔(黄色箭头),环江赖洞剖面,单偏光; b.三角形粒间孔(红色箭头),东塘1井,埋深677.2 m,扫描电镜; c.粒间溶孔(红色箭头)和粒内溶孔(黄色箭头),柳州新圩剖面,单偏光; d.粒间溶孔被片状高岭石和片丝状、毛发状伊利石集合体充填,柳州长蛇剖面,扫描电镜; e.长石颗粒溶蚀形成铸模孔(红色箭头),东塘1井,埋深660.6 m,扫描电镜;f. 长石颗粒向高岭石转化,溶蚀形成的微孔,东塘1井,埋深1 021.9 m,扫描电镜; g.多期次裂缝(红色箭头),东塘1井,埋深589.4 m,岩心; h.网状微裂缝(红色箭头),南丹地马剖面,单偏光; i.高角度缝(红色箭头),方解石半充填,东塘1井,埋深663.5 m,岩心"
图8
雪峰山南缘寺门组层序界面及沉积微相识别标志a.三级层序底界面SB1,上部为寺门组灰黑色泥岩,下部为黄金组灰黑色泥晶灰岩夹泥岩,环江塘现剖面; b.三级层序顶界面SB2,上部为罗城组灰黑色生物碎屑灰岩,下部为寺门组灰黑色泥岩,环江塘现剖面; c.四级层序MCS1与MCS2界面,上部为灰黑色泥岩,下部为灰白色石英砂岩,鹿寨石古剖面; d.四级层序MCS2与MCS3界面,上部为灰黑色泥岩,下部为浅灰色细砂岩,鹿寨石古剖面; e.泥坪微相,水平层理,环江塘现剖面; f.沿岸砂坝微相,小型交错层理,环江赖洞剖面; g.混合坪微相,透镜状、波状层理,鹿寨长胜剖面; h.砂泥质滨岸微相,泥质粉砂岩,波痕构造,东塘1井,埋深825.0 m; i.潟湖微相,以水平层理为主的复合韵律层理,东塘1井,埋深719.1 m"
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