石油与天然气地质 ›› 2022, Vol. 43 ›› Issue (6): 1397-1412.doi: 10.11743/ogg20220610
• 油气地质 • 上一篇
夏辉1,2(), 王龙1,2, 张道锋1,2, 王继平1,2, 范倩倩1,2, 冯敏1,2, 王艳1,2
收稿日期:
2022-04-10
修回日期:
2022-09-22
出版日期:
2022-12-01
发布日期:
2022-11-21
第一作者简介:
夏辉(1991—),男,博士、工程师,沉积学与储层地质学。E?mail: 基金项目:
Hui Xia1,2(), Long Wang1,2, Daofeng Zhang1,2, Jiping Wang1,2, Qianqian Fan1,2, Min Feng1,2, Yan Wang1,2
Received:
2022-04-10
Revised:
2022-09-22
Online:
2022-12-01
Published:
2022-11-21
摘要:
庆阳气田是鄂尔多斯盆天然气增储上产的潜力区,二叠系山西组1段(山1段)为其主力产层,然而其沉积演化及其控制因素等方面的认识依然不清,制约着气田的勘探开发。综合利用三维地震、测井、岩心及分析化验等资料,应用测井小波变换、INPEFA技术及Fischer图解等分析方法,对庆阳气田山1段沉积层序发育演化及其对古地貌、古水流流向和湖平面变化的响应关系开展了系统性研究。结果表明:山1段可划分为一个三级层序,由完整的水进—水退旋回构成,内部进一步划分出低位体系域、湖侵体系域及高位体系域,可识别出浅水三角洲以及湖泊等沉积体系。Fischer图解表明山1段的湖平面经历过“快速上升—缓慢下降”的变化过程,内部伴随着次级的湖平面振荡。“PA(进积—加积)—R(退积)—AP(加积—进积)”叠加序列的转变响应着沉积相的迁移演化及可容空间的变化。低位域时期,在沉积前微古地貌与沉积期古水流流向的耦合作用下,古地貌斜坡区三角洲砂岩储层广泛发育,是后期勘探开发的潜在有利区。
中图分类号:
表1
鄂尔多斯盆地庆阳气田山1段岩相组合类型"
岩相组合 | 沉积特征 | 沉积相解释 |
---|---|---|
FA1 | 厚层块状层理、板状交错层理及平行层理粗砂岩:底部见明显冲刷面,含石英砾岩,大套厚层块状粗砂岩向上粒度变细,板状交错层理、平行层理较发育,顶部为块状中砂岩 | 分流河道 |
FA2 | 中-薄层块状灰色泥岩:块状层理、水平层理泥岩或炭质泥岩,偶见泥裂构造 | 泛滥平原 |
FA3 | 厚层块状层理、平行层理、交错层理中-细砂岩:底部多见明显的冲刷面,含暗色泥砾,发育块状层理、槽状交错层理、板状交错层理、楔状交错层理、平行层理,底部为中-细砂岩,向上岩性变为细砂岩或粉砂岩 | 水下分流河道 |
FA4 | 中-薄层灰色块状层理泥岩或粉砂质泥岩:夹在大套的块状层理、平行层理、楔状交错层理及板状交错层理砂岩中间 | 分流间湾 |
FA5 | 中层平行层理、波状层理及楔状交错层理细-粗砂岩:呈反粒序,底部细粒泥质粉砂岩或粉砂岩向上粒度变粗,上部为粗砂岩 | 河口坝 |
FA6 | 中-薄层平行层理、脉状层理、沙纹层理及平行层理粉砂岩:反粒序,由粉砂岩向上变为粗砂岩,发育平行层理、脉状层理及沙纹层理 | 坝砂 |
FA7 | 薄层块状层理、平行层理细砂岩:薄层细砂岩,发育平行层理及块状层理 | 滩砂 |
FA8 | 厚层块状灰色或灰黑色泥岩:泥岩或粉砂质泥岩,以块状层理为主 | 浅湖泥 |
图6
鄂尔多斯盆地庆阳气田山1段典型岩相类型岩心照片a. 具冲刷面的含砾粗砂岩相,W15井,埋深4 246.10 m;b. 平行层理砂岩相,W8井,埋深4 422.95 m;c. 块状层理含砾砂岩相,W16井,埋深4 747.86 m;d. 槽状交错层理砂岩相,W17井,埋深4 336.08 m;e. 块状层理砂岩相,W18井,埋深4 165.76 m;f. 板状交错层理砂岩相,W19井,埋深4 230.20 m;g. 楔状交错层理砂岩相,W20井,埋深4 724.20 m;h. 平行层理粉砂岩相,W3井,埋深4 271.93 m;i. 沙纹层理粉砂岩相,W21井,埋深4 034.81 m;j. 波状层理粉砂岩相,W22井,埋深4 080.40 m;k. 脉状层理粉砂岩相,W16井,埋深4 751.89 m;l. 水平层理粉砂质泥岩相,W23井,埋深4 307.54 m;m.含植物根迹块状泥岩相,W21井,埋深4 033.04 m;n. 块状层理炭质泥岩相,W24井,埋深4 370.16 m;o. 块状层理杂色泥岩相,W25井,埋深4 327.40 m"
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