石油与天然气地质 ›› 2023, Vol. 44 ›› Issue (1): 110-124.doi: 10.11743/ogg20230109
• 油气地质 • 上一篇
张涛1(), 张亚雄1, 金晓辉1, 周雁1, 张军涛1, 谷宁1, 张威2, 王濡岳1, 鲁锴1
收稿日期:
2022-05-29
修回日期:
2022-11-20
出版日期:
2023-02-01
发布日期:
2023-01-13
第一作者简介:
张涛(1973—),男,高级工程师,碳酸盐岩沉积储层。E-mail:基金项目:
Tao ZHANG1(), Yaxiong ZHANG1, Xiaohui JIN1, Yan ZHOU1, Juntao ZHANG1, Ning GU1, Wei ZHANG2, Ruyue WANG1, Kai LU1
Received:
2022-05-29
Revised:
2022-11-20
Online:
2023-02-01
Published:
2023-01-13
摘要:
在充分调研已有成果的基础上,按照Vail经典层序地层理论,综合考虑碳酸盐岩-蒸发岩沉积学原理、台地形态、盆内和古隆起边缘岩性组合特征等,提出了鄂尔多斯盆地奥陶系马家沟组蒸发岩主要赋存于层序下部、浅水碳酸盐岩赋存于层序上部的层序地层划分模式,据此将马家沟组划分为5个三级层序。三级层序界面分别位于马(马家沟组)一段、马三段、马五10亚段、马五6亚段和马五4亚段底部,马家沟组底部和顶部为区域不整合面。在三级层序低位域的时限内,蒸发岩和碳酸盐岩在时空上呈指状交叉,蒸发岩沉积的次数与相邻碳酸盐岩地层中无沉积或间断(不整合)的次数相关,这种四级-五级的沉积间断面是层间溶蚀发育的前提条件,同时也决定了蒸发岩间烃源岩的发育位置。处于低位域的马一段、马三段、马五6亚段3套蒸发岩层系发育潜在烃源岩,主要分布在环盐湖外围洼地及盆地中心斜坡区,具有层薄、累计厚度大的特征。沉积相与多级次层序界面控制储层的发育,主要形成了2类储层:①滩相白云岩孔隙型储层,主要发育在三级-四级层序高位体系域中、上部,沉积间断面与滩相叠加区为孔隙型储层发育的有利层位;②含膏云岩中膏模溶孔型储层,主要发育在低位体系域的次级海侵期,古隆起边缘区潮坪相带是膏模孔溶蚀型储层发育层位。
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