石油与天然气地质 ›› 2022, Vol. 43 ›› Issue (5): 1180-1193.doi: 10.11743/ogg20220514
印森林1(), 陈恭洋1(
), 许长福2, 熊先钺3, 赵军2, 胡可2
收稿日期:
2021-11-05
修回日期:
2022-07-12
出版日期:
2022-10-01
发布日期:
2022-09-02
通讯作者:
陈恭洋
E-mail:yinxiang_love@qq.com;gychen8888@126.com
第一作者简介:
印森林(1983—),男,博士、副教授、博士生导师,油气田开发地质。E?mail: 基金项目:
Senlin Yin1(), Gongyang Chen1(
), Changfu Xu2, Xianyue Xiong3, Jun Zhao2, Ke Hu2
Received:
2021-11-05
Revised:
2022-07-12
Online:
2022-10-01
Published:
2022-09-02
Contact:
Gongyang Chen
E-mail:yinxiang_love@qq.com;gychen8888@126.com
摘要:
就陆相中高成熟度混积型页岩油开发而言,岩相对甜点的控制作用还不明确。以准噶尔盆地吉木萨尔凹陷二叠系芦草沟组为例,利用岩相构型分析、无人机倾斜摄影和三维地质建模等方法,结合岩心、露头、测井、分析化验和试油动态等资料,开展了岩相构型对甜点控制作用的研究。结果表明,把传统人工考察与无人机倾斜摄影技术结合起来,从井点设置、岩相参数定量刻画、格架模型和三维岩相原型模型建立等方面出发,可以表征芦草沟组露头剖面岩相构型三维空间分布特征。混积细粒储集岩岩相构型组合主要有渐变型、突变型和特殊型3类:渐变型砂体发育程度较高,形成上、下对称状岩相构型,常表现为多个相似旋回的叠置,烃源岩优质,储集层溶蚀孔隙发育,是优质甜点;突变型砂体发育程度一般,形成非对称状岩相构型,常呈多个相似旋回的叠置,烃源岩较为优质,储集层厚度薄;特殊型属于厚层碎屑岩类型,砂体发育程度高,呈单一旋回砂体叠置,储层较为致密,为相对优质甜点。储集岩岩相构型控制了甜点分布,并影响着开发部署策略。渐变型甜点发育程度高,非均质性弱,开发效果最好,采用大规模水平井平台化作业进行效益开发;突变型非均质性强,开发效果一般,是后续接替区域;特殊型整体呈分散状,连续性较差,非均质性强,需精细研究岩相构型空间分布,结合核磁共振法所测的物性参数和含油气性参数部署水平井开发。
中图分类号:
图9
吉木萨尔凹陷不同类型甜点储层微观孔隙特征照片a.孔隙结构较好的长石岩屑粉细砂岩,铸体薄片,P2l2(2-2),J174井,埋深3 127.53 m; b.孔隙结构较好的石英粉砂岩,铸体薄片,P2l2(2-2),J301井,埋深2 769.64 m; c.孔隙结构很好的白云质粉砂岩,铸体薄片,P2l1(2-2),J174井,埋深3 276.15 m; d.富含有机质的粉砂质泥岩,普通薄片,P2l2(2-1),J174井,埋深3 109.22 m; e.溶蚀孔隙发育的砂屑云岩,铸体薄片,P2l2(2-1),J174井,埋深3 112.09 m; f.泥晶/微晶白云岩,普通薄片,P2l2(2-3),J174井,埋深3 145.19 m; g.不同含油级别呈纹层状互层(对应d图,TOC为10.85 %),荧光扫描,J174井,第4筒2/55; h.荧光扫描砂屑白云岩不敏感(对应e图,TOC为0.85 %),荧光扫描,J174井,第4筒22/55; i.含油气级别中等(对应f图,TOC为3.71 %),J174井,第8筒2-4/45"
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