同生逆断层控制的砂砾岩沉积模式及有利储集相带分布&mdash;&mdash;以玛湖凹陷南斜坡白25井区上乌尔禾组为例

孟祥超; 蒋庆平; 李亚哲; 孔垂显; 吴爱成; 王力宝; 贾俊飞; 肖芳伟; 刘午牛

doi:10.14027/j.cnki.cjxb.2017.06.014

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

同生逆断层控制的砂砾岩沉积模式及有利储集相带分布——以玛湖凹陷南斜坡白25井区上乌尔禾组为例

孟祥超, 蒋庆平, 李亚哲, 孔垂显, 吴爱成, 王力宝, 贾俊飞, 肖芳伟, 刘午牛

文章导航 > 沉积学报 > 2017 > 35(6): 1225-1240

孟祥超, 蒋庆平, 李亚哲, 孔垂显, 吴爱成, 王力宝, 贾俊飞, 肖芳伟, 刘午牛. 同生逆断层控制的砂砾岩沉积模式及有利储集相带分布——以玛湖凹陷南斜坡白25井区上乌尔禾组为例[J]. 沉积学报, 2017, 35(6): 1225-1240. doi: 10.14027/j.cnki.cjxb.2017.06.014

引用本文:

MENG XiangChao, JIANG QingPing, LI YaZhe, KONG ChuiXian, WU AiCheng, WANG LiBao, JIA JunFei, XIAO FangWei, LIU WuNiu. Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P3w, B25 Block, Mahu sag, as an example[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1225-1240. doi: 10.14027/j.cnki.cjxb.2017.06.014

Citation:

MENG XiangChao, JIANG QingPing, LI YaZhe, KONG ChuiXian, WU AiCheng, WANG LiBao, JIA JunFei, XIAO FangWei, LIU WuNiu. Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P₃w, B25 Block, Mahu sag, as an example[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1225-1240. doi: 10.14027/j.cnki.cjxb.2017.06.014

引用本文:

Citation:

MENG XiangChao, JIANG QingPing, LI YaZhe, KONG ChuiXian, WU AiCheng, WANG LiBao, JIA JunFei, XIAO FangWei, LIU WuNiu. Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P₃w, B25 Block, Mahu sag, as an example[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1225-1240. doi: 10.14027/j.cnki.cjxb.2017.06.014

同生逆断层控制的砂砾岩沉积模式及有利储集相带分布——以玛湖凹陷南斜坡白25井区上乌尔禾组为例

doi: 10.14027/j.cnki.cjxb.2017.06.014

1.
中国石油杭州地质研究院, 杭州 310023;
2.
新疆油田公司勘探开发研究院, 新疆克拉玛依 834000

基金项目: 中油股份公司<新疆大庆>科技攻关项目（HX132-41528-15）

详细信息

作者简介:
孟祥超,男,1974年出生,高级工程师,沉积储层,E-mail:mengxc_hz@petrochina.com.cn

中图分类号: P512.2

计量

文章访问数: 441
HTML全文浏览量: 96
PDF下载量: 697
被引次数: 0

Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P₃w, B25 Block, Mahu sag, as an example

1.
Hangzhou Research Institute of Petroleum Geology, CNPC, Zhejiang, Hangzhou 310023, China;
2.
Xinjiang Oilfield Company Exploration and Development Research Institute, CNPC, Xinjiang, Karamay, Xinjiang 834000, China

Funds: Science and Technology Key Project,CNPC,No.HX132-41528-15

摘要

摘要: 通过岩芯相-测井相-地震相-分析化验数据对比，结合砂砾岩沉积野外考察实践综合归纳分析，认为上乌尔禾组同生逆断层控制的冲积扇-扇三角洲砂砾岩沉积体系整体呈进积式沉积，具"冲积扇扇根（槽流带）-冲积扇扇中/扇三角洲平原（辫流带）-扇三角洲前缘（水下分流带）-前扇三角洲/滨浅湖（夹杂水下扇）"相序特征，发育槽流、泥石流/砂质碎屑流、辫状河道、水下分流河道、扇面水道五种典型砂砾岩沉积微相类型。同生逆断层带不断抬升剥蚀的累积效应，使近物源区冲积扇扇根沉积整体减薄，同时使同生逆断层控制沉积相带分异的趋势越来越明显。泥质含量是控制挤压背景下砂砾岩储层质量的关键因素，贫泥砂砾岩储层成岩压实减孔效应弱，剩余粒间孔发育，且粗粒级颗粒内部多发育压碎缝沟通粒间孔隙，储层质量最佳。依据储集空间组合类型将有利储集相带分为原生粒间孔-压碎缝发育带、原生粒间孔-次生溶孔发育带两大类。前者主要分布于构造高部位近断裂带-中上斜坡带；后者主要分布于中下部斜坡带。
- 玛湖凹陷南斜坡 /
- 上乌尔禾组 /
- 冲积扇 /
- 扇三角洲 /
- 同生逆断层 /
- 泥质含量 /
- 压碎缝
Abstract: Based on the analysis of core facies, logging facies, seismic facies and analysis assay data, with the field practice induction of glutenite sedimentary,this paper draw conclusions that:Fan-fan delta glutenite sedimentary system under the control of contemporaneous reverse thrust show the progradation deposition on the whole in P₃w. Indicating the phase-sequence characteristics called "Alluvial fan toe (channel flow)-Alluvial fan middle/Fan delta plain (braided stream)-Fan delta front(distributary belt)-former fan delta/shallow lake (be mixed up with subaqueous fan)".with the development of such five typical glutenite sedimentary microfacies types as channel flow, debris flow/sandy debris flow, braided channel, underwater distributary channel, sectoral waterway. The cumulative effect of contemporaneous reverse fault belt continuous uplifting and denudation, make the sedimentary of fan toe in alluvial fan thinning, with more and more obvious trend of contemporaneous reverse fault controlling the sedimentary facies differentiation. Shale content is the key control factors of glutenite reservoir quality under the extrusion background. The diagenetic compaction cut hole effect in poor mud glutenite reservoir is weak, with the higher residual intergranular pore development and the higher development level of crush seam in coarse particles communicating intergranular pore, the reservoir quality of poor mud glutenite is best. Based on combination of reservoir space,the favorable reservoir facies belt can be divided into two types:primary intergranular pore-crush seam development zones and primary intergranular pore-secondary dissolution pore development zones. The former mainly distributed in the fault zone-upper slope belt near structural high position, the latter mainly distributed in middle-lower slope belt.
- south slope in Mahu sag /
- P₃w /
- alluvial fan /
- fan delta /
- contemporaneous reverse fault /
- shale content /
- crush seam

HTML全文

参考文献(0)

[1]	高志勇, 冯佳睿, 石雨昕, 罗忠, 张宇航. 干旱气候下冲积扇—冲积平原曲流河沉积演化过程与展布 . 沉积学报, 2023, 41(6): 1954-1970. doi: 10.14027/j.issn.1000-0550.2022.122
[2]	单祥. 准噶尔盆地阜康凹陷深层二叠系上乌尔禾组致密砂砾岩储层特征、成因及勘探方向 . 沉积学报, 2023, (): -. doi: 10.14027/j.issn.1000-0550.2023.097
[3]	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
[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]	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
[6]	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
[7]	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
[8]	高志勇, 石雨昕, 周川闽, 冯佳睿, 翟羿程, 樊小容. 砾石分析在扇三角洲与湖岸线演化关系中的应用——以准噶尔盆地玛湖凹陷周缘百口泉组为例 . 沉积学报, 2019, 37(3): 550-564. doi: 10.14027/j.issn.1000-0550.2019.005
[9]	印森林, 刘忠保, 陈燕辉, 吴小军. 冲积扇研究现状及沉积模拟实验——以碎屑流和辫状河共同控制的冲积扇为例 . 沉积学报, 2017, 35(1): 10-23. doi: 10.14027/j.cnki.cjxb.2017.01.002
[10]	赖海成, 李志忠, 靳建辉, 邓涛, 姜锋, 于晓莉, 苑秀全, 申健玲, 龚松柏. 基于GPR图像的福建海坛岛北部海岸冲积扇沉积构造及其成因的初步研究 . 沉积学报, 2016, 34(4): 645-652. doi: 10.14027/j.cnki.cjxb.2016.04.004
[11]	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
[12]	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.
[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]	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.
[15]	郭建华, 朱美衡, 杨申谷, 刘辰生. 辽河盆地曙一区馆陶组湿地冲积扇沉积 . 沉积学报, 2003, 21(3): 367-372.
[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]	吴智勇, 郭建华, 吴东胜, 何宏. 东濮断陷湖盆下第三系沙二段的冲积扇沉积 . 沉积学报, 1999, 17(3): 449-453.
[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]	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.
[20]	柯保嘉, 陈昌明, 陈志明, 汪寿松, 姜好仁, 惠斌耀. 鄂尔多斯盆地西缘砾质冲积扇沉积学特征 . 沉积学报, 1991, 9(3): 11-21.

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: 441
HTML全文浏览量: 96
PDF下载量: 697
被引次数: 0

同生逆断层控制的砂砾岩沉积模式及有利储集相带分布——以玛湖凹陷南斜坡白25井区上乌尔禾组为例

doi: 10.14027/j.cnki.cjxb.2017.06.014

1. 中国石油杭州地质研究院, 杭州 310023;

2. 新疆油田公司勘探开发研究院, 新疆克拉玛依 834000

基金项目: 中油股份公司<新疆大庆>科技攻关项目（HX132-41528-15）

作者简介:
孟祥超,男,1974年出生,高级工程师,沉积储层,E-mail:mengxc_hz@petrochina.com.cn

收稿日期: 2016-09-20
修回日期: 2016-11-22
刊出日期: 2017-12-10

中图分类号: P512.2

关键词:

冲积扇 /

摘要: 通过岩芯相-测井相-地震相-分析化验数据对比，结合砂砾岩沉积野外考察实践综合归纳分析，认为上乌尔禾组同生逆断层控制的冲积扇-扇三角洲砂砾岩沉积体系整体呈进积式沉积，具"冲积扇扇根（槽流带）-冲积扇扇中/扇三角洲平原（辫流带）-扇三角洲前缘（水下分流带）-前扇三角洲/滨浅湖（夹杂水下扇）"相序特征，发育槽流、泥石流/砂质碎屑流、辫状河道、水下分流河道、扇面水道五种典型砂砾岩沉积微相类型。同生逆断层带不断抬升剥蚀的累积效应，使近物源区冲积扇扇根沉积整体减薄，同时使同生逆断层控制沉积相带分异的趋势越来越明显。泥质含量是控制挤压背景下砂砾岩储层质量的关键因素，贫泥砂砾岩储层成岩压实减孔效应弱，剩余粒间孔发育，且粗粒级颗粒内部多发育压碎缝沟通粒间孔隙，储层质量最佳。依据储集空间组合类型将有利储集相带分为原生粒间孔-压碎缝发育带、原生粒间孔-次生溶孔发育带两大类。前者主要分布于构造高部位近断裂带-中上斜坡带；后者主要分布于中下部斜坡带。

English Abstract

Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P₃w, B25 Block, Mahu sag, as an example

1. Hangzhou Research Institute of Petroleum Geology, CNPC, Zhejiang, Hangzhou 310023, China;

2. Xinjiang Oilfield Company Exploration and Development Research Institute, CNPC, Xinjiang, Karamay, Xinjiang 834000, China

Funds: Science and Technology Key Project,CNPC,No.HX132-41528-15

Received Date: 2016-09-20
Rev Recd Date: 2016-11-22
Publish Date: 2017-12-10

Keywords:

Abstract: Based on the analysis of core facies, logging facies, seismic facies and analysis assay data, with the field practice induction of glutenite sedimentary,this paper draw conclusions that:Fan-fan delta glutenite sedimentary system under the control of contemporaneous reverse thrust show the progradation deposition on the whole in P₃w. Indicating the phase-sequence characteristics called "Alluvial fan toe (channel flow)-Alluvial fan middle/Fan delta plain (braided stream)-Fan delta front(distributary belt)-former fan delta/shallow lake (be mixed up with subaqueous fan)".with the development of such five typical glutenite sedimentary microfacies types as channel flow, debris flow/sandy debris flow, braided channel, underwater distributary channel, sectoral waterway. The cumulative effect of contemporaneous reverse fault belt continuous uplifting and denudation, make the sedimentary of fan toe in alluvial fan thinning, with more and more obvious trend of contemporaneous reverse fault controlling the sedimentary facies differentiation. Shale content is the key control factors of glutenite reservoir quality under the extrusion background. The diagenetic compaction cut hole effect in poor mud glutenite reservoir is weak, with the higher residual intergranular pore development and the higher development level of crush seam in coarse particles communicating intergranular pore, the reservoir quality of poor mud glutenite is best. Based on combination of reservoir space,the favorable reservoir facies belt can be divided into two types:primary intergranular pore-crush seam development zones and primary intergranular pore-secondary dissolution pore development zones. The former mainly distributed in the fault zone-upper slope belt near structural high position, the latter mainly distributed in middle-lower slope belt.

引用本文:

Citation:

MENG XiangChao, JIANG QingPing, LI YaZhe, KONG ChuiXian, WU AiCheng, WANG LiBao, JIA JunFei, XIAO FangWei, LIU WuNiu. Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P₃w, B25 Block, Mahu sag, as an example[J]. Acta Sedimentologica Sinica, 2017, 35(6): 1225-1240. doi: 10.14027/j.cnki.cjxb.2017.06.014

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

同生逆断层控制的砂砾岩沉积模式及有利储集相带分布——以玛湖凹陷南斜坡白25井区上乌尔禾组为例

doi: 10.14027/j.cnki.cjxb.2017.06.014

作者简介:
孟祥超,男,1974年出生,高级工程师,沉积储层,E-mail:mengxc_hz@petrochina.com.cn

计量

Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P₃w, B25 Block, Mahu sag, as an example

计量

目录

同生逆断层控制的砂砾岩沉积模式及有利储集相带分布——以玛湖凹陷南斜坡白25井区上乌尔禾组为例

doi: 10.14027/j.cnki.cjxb.2017.06.014

1. 中国石油杭州地质研究院, 杭州 310023;

2. 新疆油田公司勘探开发研究院, 新疆克拉玛依 834000

作者简介:
孟祥超,男,1974年出生,高级工程师,沉积储层,E-mail:mengxc_hz@petrochina.com.cn

English Abstract

Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P₃w, B25 Block, Mahu sag, as an example

1. Hangzhou Research Institute of Petroleum Geology, CNPC, Zhejiang, Hangzhou 310023, China;

2. Xinjiang Oilfield Company Exploration and Development Research Institute, CNPC, Xinjiang, Karamay, Xinjiang 834000, China

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

同生逆断层控制的砂砾岩沉积模式及有利储集相带分布——以玛湖凹陷南斜坡白25井区上乌尔禾组为例

doi: 10.14027/j.cnki.cjxb.2017.06.014

作者简介: 孟祥超,男,1974年出生,高级工程师,沉积储层,E-mail:mengxc_hz@petrochina.com.cn

计量

出版历程

Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P3w, B25 Block, Mahu sag, as an example

计量

出版历程

目录

同生逆断层控制的砂砾岩沉积模式及有利储集相带分布——以玛湖凹陷南斜坡白25井区上乌尔禾组为例

doi: 10.14027/j.cnki.cjxb.2017.06.014

1. 中国石油杭州地质研究院, 杭州 310023; 2. 新疆油田公司勘探开发研究院, 新疆克拉玛依 834000

作者简介: 孟祥超,男,1974年出生,高级工程师,沉积储层,E-mail:mengxc_hz@petrochina.com.cn

English Abstract

Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P3w, B25 Block, Mahu sag, as an example

1. Hangzhou Research Institute of Petroleum Geology, CNPC, Zhejiang, Hangzhou 310023, China; 2. Xinjiang Oilfield Company Exploration and Development Research Institute, CNPC, Xinjiang, Karamay, Xinjiang 834000, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
孟祥超,男,1974年出生,高级工程师,沉积储层,E-mail:mengxc_hz@petrochina.com.cn

Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P₃w, B25 Block, Mahu sag, as an example

1. 中国石油杭州地质研究院, 杭州 310023;

2. 新疆油田公司勘探开发研究院, 新疆克拉玛依 834000

作者简介:
孟祥超,男,1974年出生,高级工程师,沉积储层,E-mail:mengxc_hz@petrochina.com.cn

Glutenite Sedimentary Pattern under the Control of Contemporaneous Reverse Thrust and Favorable Reservoir Facies Belt Distribution-Taking P₃w, B25 Block, Mahu sag, as an example

1. Hangzhou Research Institute of Petroleum Geology, CNPC, Zhejiang, Hangzhou 310023, China;

2. Xinjiang Oilfield Company Exploration and Development Research Institute, CNPC, Xinjiang, Karamay, Xinjiang 834000, China