涠西南凹陷涠洲10-3油田及围区流三段沉积相研究

李茂; 董桂玉; 漆智

doi:10.14027/j.cnki.cjxb.2015.02.011

ISSN 1000-0550 CN 62-1038/P

高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

涠西南凹陷涠洲10-3油田及围区流三段沉积相研究

李茂, 董桂玉, 漆智

文章导航 > 沉积学报 > 2015 > 33(2): 314-325

李茂, 董桂玉, 漆智. 涠西南凹陷涠洲10-3油田及围区流三段沉积相研究[J]. 沉积学报, 2015, 33(2): 314-325. doi: 10.14027/j.cnki.cjxb.2015.02.011

引用本文:

李茂, 董桂玉, 漆智. 涠西南凹陷涠洲10-3油田及围区流三段沉积相研究[J]. 沉积学报, 2015, 33(2): 314-325. doi: 10.14027/j.cnki.cjxb.2015.02.011

LI Mao, DONG GuiYu, QI Zhi. Sedimentary Facies of Member 3 of Liushagang Formation of WZ10-3 Oilfield and Surrounding Areas in Weixinan Sag[J]. Acta Sedimentologica Sinica, 2015, 33(2): 314-325. doi: 10.14027/j.cnki.cjxb.2015.02.011

Citation:

LI Mao, DONG GuiYu, QI Zhi. Sedimentary Facies of Member 3 of Liushagang Formation of WZ10-3 Oilfield and Surrounding Areas in Weixinan Sag[J]. Acta Sedimentologica Sinica, 2015, 33(2): 314-325. doi: 10.14027/j.cnki.cjxb.2015.02.011

李茂, 董桂玉, 漆智. 涠西南凹陷涠洲10-3油田及围区流三段沉积相研究[J]. 沉积学报, 2015, 33(2): 314-325. doi: 10.14027/j.cnki.cjxb.2015.02.011

引用本文:

李茂, 董桂玉, 漆智. 涠西南凹陷涠洲10-3油田及围区流三段沉积相研究[J]. 沉积学报, 2015, 33(2): 314-325. doi: 10.14027/j.cnki.cjxb.2015.02.011

Citation:

涠西南凹陷涠洲10-3油田及围区流三段沉积相研究

doi: 10.14027/j.cnki.cjxb.2015.02.011

李茂^1,2,
董桂玉³,
漆智²

1.
中国地质大学(武汉)资源学院武汉 430074;
2.
中海石油(中国)有限公司湛江分公司广东湛江 524057;
3.
河北联合大学矿业工程学院河北唐山 063009

基金项目: 中海石油(中国)有限公司自有综合课题项目"涠西南凹陷流三段储层综合评价技术研究"(编号:ZYKY-2012-ZJ-02)资助

详细信息

中图分类号: TE122.2

计量

文章访问数: 949
HTML全文浏览量: 47
PDF下载量: 2699
被引次数: 0

Sedimentary Facies of Member 3 of Liushagang Formation of WZ10-3 Oilfield and Surrounding Areas in Weixinan Sag

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074;
2.
Zhanjiang Division of CNOOC Ltd., Zhanjiang, Guangdong 524057;
3.
School of Mineral Engineering, Hebei United University, Tangshan, Hebei 063009

摘要

摘要: 为了促进涠西南凹陷涠洲10-3油田及围区流三段油藏的滚动勘探开发,开展了油区沉积相精细研究。利用岩芯、录井、测井和地震等资料,在识别不同级别层序界面和湖泛面的基础上,将涠洲10-3油田及围区流三段划分为2个长期基准面旋回和8个中期基准面旋回,建立了高分辨率层序地层对比格架。在岩芯描述基础上,进行单井沉积相、连井沉积相、平面沉积相分析,认为研究区流三段发育冲积扇、扇三角洲和湖泊3种沉积相,并系统划分了沉积微相类型。探讨了碎屑流沉积的相带归属,将发育在河道中的碎屑流沉积划分为河道型碎屑流沉积,将单独产出的碎屑流沉积根据沉积环境不同划分为水上非河道化碎屑流沉积和水下非河道化碎屑流沉积。最后对各中期基准面旋回的沉积相展布特征和演化规律进行了探讨,并建立了符合研究区的沉积相模式。
- 涠洲10-3油田 /
- 流三段 /
- 高分辨率层序地层 /
- 沉积相 /
- 扇三角洲 /
- 碎屑流沉积
Abstract: In order to promote progressive exploration and development in WZ10-3 Oilfield and surrounding area, the fine sedimentary facies study in oil region was carried out. Guided by the high resolution sequence stratigraphy theory, in combination with core, logging, log and seismic data, on the basis of recognition of different levels sequence interfaces and the types of maximum lake flooding surface, the Member 3 of Liushagang Formation can be divided into two long-term base level cyclical sequence and eight middle-term base level cyclical sequence. By analyses of individual well sedimentary facies, section sedimentary facies and plane sedimentary facies, 3 sedimentary facies of alluvial fan, fan delta and lacustine were identified in the Member 3 of Liushagang Formation, and microfacies were divided, facies belt ownership of debris flow deposit was discussed systematically. Debris flow deposits developing in channels were divided into 3 types, i.e., channels, distribution channels and subaqueous distribution channels microfacies. While individual developmental debris flow deposits were divided into 2 types, i.e., subaerial non-channelized and subaqueous non-channelized debris flows microfacies. On the basis of these, sedimentary facies distribution and sedimentary evolution rule of MSC1 to MSC8 of the Member 3 of Liushagang Formation were discussed, and sedimentary models were established finally.
- Weixinan sag /
- WZ10-3 Oilfield /
- member 3 of Liushagang Formation /
- high-resolution sequence stratigraphy /
- sedimentary facies /
- fan delta

HTML全文

参考文献(0)

[1]	陈彬滔, 马轮, 洪亮, 史忠生, 庞文珠, 薛罗, 王磊, 代寒松, 赵艳军. 断陷湖盆陡坡带扇三角洲—滑塌扇复合扇体的沉积演化及油气地质意义 . 沉积学报, 2024, 42(3): 1058-1072. doi: 10.14027/j.issn.1000-0550.2022.087
[2]	周振永, 李德勇, 段驰宇, 任操, 揭琼, 戴明辉, 程宏岗. 廊固凹陷扇三角洲沉积及成藏模式—— 以旧州-万庄地区沙河街组为例 . 沉积学报, 2023, (): -. doi: 10.14027/j.issn.1000-0550.2023.079
[3]	陶金雨, 张昌民, 郭旭光, 朱锐, 潘进, 唐勇. 磨圆度定量表征在扇三角洲沉积微相判别中的应用 . 沉积学报, 2020, 38(5): 956-965. doi: 10.14027/j.issn.1000-0550.2019.111
[4]	何岸北, 胡煜昭, 任涛, 董传奇, 刘昌伟, 张宇寒. 新疆乌拉根铅锌矿克五段扇三角洲沉积模式 . 沉积学报, 2020, 38(2): 245-256. doi: 10.14027/j.issn.1000-0550.2019.028
[5]	蒋庆平, 孔垂显, 李维锋, 邱子刚, 卢志远, 常天全, 刘凯, 陈栋梁, 李胜, 袁晓光. 陆相湖盆大型扇三角洲沉积特征与演化规律 . 沉积学报, 2020, 38(5): 923-932. doi: 10.14027/j.issn.1000-0550.2019.089
[6]	王越. 新疆塔尔朗沟剖面中二叠统扇三角洲混合沉积特征及模式 . 沉积学报, 2019, 37(5): 922-933. doi: 10.14027/j.issn.1000-0550.2018.190
[7]	周学文, 姜在兴, 汤望新, 许文茂, 胡晨林, 贾超尘. 牛庄洼陷沙三中亚段三角洲—重力流体系沉积特征与模式 . 沉积学报, 2018, 36(2): 376-389. doi: 10.14027/j.issn.1000-0550.2018.027
[8]	邹妞妞, 史基安, 张大权, 马崇尧, 张顺存, 鲁新川. 准噶尔盆地西北缘玛北地区百口泉组扇三角洲沉积模式 . 沉积学报, 2015, 33(3): 607-615. doi: 10.14027/j.cnki.cjxb.2015.03.019
[9]	汪满福. 酒泉盆地青西凹陷下沟组高分辨率层序分析 . 沉积学报, 2008, 26(4): 624-631.
[10]	肖〓毅. 辽河清水洼陷东营组高分辨率层序格架下沉积演化特征及有利区带预测 . 沉积学报, 2008, 26(6): 1014-1020.
[11]	魏钦廉. 惠州凹陷古近系珠海组海相三角洲高分辨率层序地层学研究 . 沉积学报, 2008, 26(5): 744-752.
[12]	高剑波, 钟建华, 徐小林, 温志峰, 黄立功, 刘云田, 江波. 阿尔金断裂为边界的盆地斜坡带扇三角洲 . 沉积学报, 2004, 22(2): 206-215.
[13]	鄢继华, 陈世悦, 程立华. 扇三角洲亚相定量划分的思考 . 沉积学报, 2004, 22(3): 443-448.
[14]	赵俊青, 纪友亮, 夏斌, 张善文, 刘宝明. 扇三角洲沉积体系高精度层序地层学研究 . 沉积学报, 2004, 22(2): 302-309.
[15]	刘星, 陆友明, 程守田, 胡光道. 垦西油田馆陶组河流沉积高分辨率层序地层研究 . 沉积学报, 2002, 20(1): 101-105,111.
[16]	张春生, 刘忠保, 施冬, 贾爱林. 扇三角洲形成过程及演变规律 . 沉积学报, 2000, 18(4): 521-526.
[17]	刘志飞, 王成善. 西藏日喀则地区早白垩世恰布林组辫状河—扇三角洲沉积 . 沉积学报, 1998, 16(3): 6-13.
[18]	李文厚. 塔西南坳陷侏罗系的扇三角洲沉积 . 沉积学报, 1998, 16(2): 150-154.
[19]	李文厚, 林晋炎, 袁明生, 王武和. 吐鲁番－哈密盆地的两种粗碎屑三角洲 . 沉积学报, 1996, 14(3): 113-121.
[20]	顾家裕, 何斌. 塔里木盆地轮南地区三叠系扇三角洲沉积与储集层研究 . 沉积学报, 1994, 12(2): 54-62.

施引文献

资源附件(0)

访问统计

点击查看大图

计量

文章访问数: 949
HTML全文浏览量: 47
PDF下载量: 2699
被引次数: 0

涠西南凹陷涠洲10-3油田及围区流三段沉积相研究

doi: 10.14027/j.cnki.cjxb.2015.02.011

1. 中国地质大学(武汉)资源学院武汉 430074;

2. 中海石油(中国)有限公司湛江分公司广东湛江 524057;

3. 河北联合大学矿业工程学院河北唐山 063009

基金项目: 中海石油(中国)有限公司自有综合课题项目"涠西南凹陷流三段储层综合评价技术研究"(编号:ZYKY-2012-ZJ-02)资助

收稿日期: 2014-03-17
修回日期: 2014-06-18
刊出日期: 2015-04-10

中图分类号: TE122.2

关键词:

流三段 /

沉积相 /

摘要: 为了促进涠西南凹陷涠洲10-3油田及围区流三段油藏的滚动勘探开发,开展了油区沉积相精细研究。利用岩芯、录井、测井和地震等资料,在识别不同级别层序界面和湖泛面的基础上,将涠洲10-3油田及围区流三段划分为2个长期基准面旋回和8个中期基准面旋回,建立了高分辨率层序地层对比格架。在岩芯描述基础上,进行单井沉积相、连井沉积相、平面沉积相分析,认为研究区流三段发育冲积扇、扇三角洲和湖泊3种沉积相,并系统划分了沉积微相类型。探讨了碎屑流沉积的相带归属,将发育在河道中的碎屑流沉积划分为河道型碎屑流沉积,将单独产出的碎屑流沉积根据沉积环境不同划分为水上非河道化碎屑流沉积和水下非河道化碎屑流沉积。最后对各中期基准面旋回的沉积相展布特征和演化规律进行了探讨,并建立了符合研究区的沉积相模式。

English Abstract

Sedimentary Facies of Member 3 of Liushagang Formation of WZ10-3 Oilfield and Surrounding Areas in Weixinan Sag

1. School of Earth Resources, China University of Geosciences, Wuhan 430074;

2. Zhanjiang Division of CNOOC Ltd., Zhanjiang, Guangdong 524057;

3. School of Mineral Engineering, Hebei United University, Tangshan, Hebei 063009

Received Date: 2014-03-17
Rev Recd Date: 2014-06-18
Publish Date: 2015-04-10

Keywords:

Abstract: In order to promote progressive exploration and development in WZ10-3 Oilfield and surrounding area, the fine sedimentary facies study in oil region was carried out. Guided by the high resolution sequence stratigraphy theory, in combination with core, logging, log and seismic data, on the basis of recognition of different levels sequence interfaces and the types of maximum lake flooding surface, the Member 3 of Liushagang Formation can be divided into two long-term base level cyclical sequence and eight middle-term base level cyclical sequence. By analyses of individual well sedimentary facies, section sedimentary facies and plane sedimentary facies, 3 sedimentary facies of alluvial fan, fan delta and lacustine were identified in the Member 3 of Liushagang Formation, and microfacies were divided, facies belt ownership of debris flow deposit was discussed systematically. Debris flow deposits developing in channels were divided into 3 types, i.e., channels, distribution channels and subaqueous distribution channels microfacies. While individual developmental debris flow deposits were divided into 2 types, i.e., subaerial non-channelized and subaqueous non-channelized debris flows microfacies. On the basis of these, sedimentary facies distribution and sedimentary evolution rule of MSC1 to MSC8 of the Member 3 of Liushagang Formation were discussed, and sedimentary models were established finally.

李茂, 董桂玉, 漆智. 涠西南凹陷涠洲10-3油田及围区流三段沉积相研究[J]. 沉积学报, 2015, 33(2): 314-325. doi: 10.14027/j.cnki.cjxb.2015.02.011

引用本文:

李茂, 董桂玉, 漆智. 涠西南凹陷涠洲10-3油田及围区流三段沉积相研究[J]. 沉积学报, 2015, 33(2): 314-325. doi: 10.14027/j.cnki.cjxb.2015.02.011

Citation:

全文HTML

下载: 全尺寸图片幻灯片

返回文章

用微信扫码二维码

分享至好友和朋友圈

x 关闭永久关闭

2023年地质事件沉积研究新进展国际学术研讨会（第一号通知）

留言板

涠西南凹陷涠洲10-3油田及围区流三段沉积相研究

doi: 10.14027/j.cnki.cjxb.2015.02.011

计量

Sedimentary Facies of Member 3 of Liushagang Formation of WZ10-3 Oilfield and Surrounding Areas in Weixinan Sag

计量

目录

涠西南凹陷涠洲10-3油田及围区流三段沉积相研究

doi: 10.14027/j.cnki.cjxb.2015.02.011

1. 中国地质大学(武汉)资源学院武汉 430074;

2. 中海石油(中国)有限公司湛江分公司广东湛江 524057;

3. 河北联合大学矿业工程学院河北唐山 063009

English Abstract

Sedimentary Facies of Member 3 of Liushagang Formation of WZ10-3 Oilfield and Surrounding Areas in Weixinan Sag

1. School of Earth Resources, China University of Geosciences, Wuhan 430074;

2. Zhanjiang Division of CNOOC Ltd., Zhanjiang, Guangdong 524057;

3. School of Mineral Engineering, Hebei United University, Tangshan, Hebei 063009

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

涠西南凹陷涠洲10-3油田及围区流三段沉积相研究

doi: 10.14027/j.cnki.cjxb.2015.02.011

计量

出版历程

Sedimentary Facies of Member 3 of Liushagang Formation of WZ10-3 Oilfield and Surrounding Areas in Weixinan Sag

计量

出版历程

目录

涠西南凹陷涠洲10-3油田及围区流三段沉积相研究

doi: 10.14027/j.cnki.cjxb.2015.02.011

1. 中国地质大学(武汉)资源学院 武汉 430074; 2. 中海石油(中国)有限公司湛江分公司 广东湛江 524057; 3. 河北联合大学矿业工程学院 河北唐山 063009

English Abstract

Sedimentary Facies of Member 3 of Liushagang Formation of WZ10-3 Oilfield and Surrounding Areas in Weixinan Sag

1. School of Earth Resources, China University of Geosciences, Wuhan 430074; 2. Zhanjiang Division of CNOOC Ltd., Zhanjiang, Guangdong 524057; 3. School of Mineral Engineering, Hebei United University, Tangshan, Hebei 063009

全文HTML

目录

友情链接

期刊在线

联系我们

1. 中国地质大学(武汉)资源学院武汉 430074;

2. 中海石油(中国)有限公司湛江分公司广东湛江 524057;

3. 河北联合大学矿业工程学院河北唐山 063009

1. School of Earth Resources, China University of Geosciences, Wuhan 430074;

2. Zhanjiang Division of CNOOC Ltd., Zhanjiang, Guangdong 524057;

3. School of Mineral Engineering, Hebei United University, Tangshan, Hebei 063009