砂砾岩沉积特征分析及有利储集相带确定&mdash;&mdash;以玛北斜坡区百口泉组为例

孟祥超; 陈能贵; 王海明; 徐洋; 谢宗瑞; 邹志文; 郭华军; 李亚哲

doi:10.14027/j.cnki.cjxb.2015.06.016

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砂砾岩沉积特征分析及有利储集相带确定——以玛北斜坡区百口泉组为例

孟祥超, 陈能贵, 王海明, 徐洋, 谢宗瑞, 邹志文, 郭华军, 李亚哲

文章导航 > 沉积学报 > 2015 > 33(6): 1235-1246

孟祥超, 陈能贵, 王海明, 徐洋, 谢宗瑞, 邹志文, 郭华军, 李亚哲. 砂砾岩沉积特征分析及有利储集相带确定——以玛北斜坡区百口泉组为例[J]. 沉积学报, 2015, 33(6): 1235-1246. doi: 10.14027/j.cnki.cjxb.2015.06.016

引用本文:

MENG XiangChao, CHEN NengGui, WANG HaiMing, XU Yang, XIE ZongRui, ZOU ZhiWen, GUO HuaJun, LI YaZhe. Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T1b, Mabei Slope, Junggar Basin[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1235-1246. doi: 10.14027/j.cnki.cjxb.2015.06.016

Citation:

MENG XiangChao, CHEN NengGui, WANG HaiMing, XU Yang, XIE ZongRui, ZOU ZhiWen, GUO HuaJun, LI YaZhe. Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T₁b, Mabei Slope, Junggar Basin[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1235-1246. doi: 10.14027/j.cnki.cjxb.2015.06.016

引用本文:

Citation:

MENG XiangChao, CHEN NengGui, WANG HaiMing, XU Yang, XIE ZongRui, ZOU ZhiWen, GUO HuaJun, LI YaZhe. Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T₁b, Mabei Slope, Junggar Basin[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1235-1246. doi: 10.14027/j.cnki.cjxb.2015.06.016

砂砾岩沉积特征分析及有利储集相带确定——以玛北斜坡区百口泉组为例

doi: 10.14027/j.cnki.cjxb.2015.06.016

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: <新疆大庆>科技攻关项目"玛北斜坡区百口泉组沉积相研究及储层精细描述"(编号:HX132-11311)资助

详细信息

作者简介:
孟祥超男 1974年出生硕士高级工程师沉积储层 E-mail:mengxc_hz@petrochina.com.cn

中图分类号: P618.13

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PDF下载量: 407
被引次数: 0

Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T₁b, Mabei Slope, Junggar Basin

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

摘要

摘要: 为明确砂砾岩复杂储层的沉积特征及有利储集相带分布,通过岩心、测井、地震、实验分析等资料综合研究,认为玛北斜坡区百口泉组属近源快速堆积的扇三角洲沉积体系,主要发育扇三角洲平原辫状河道、扇三角洲平原/前缘砂质碎屑流、扇三角洲前缘近岸水下分流河道、远岸水下分流河道、河口坝五种主要沉积微相类型。发育牵引流、重力流两种搬运机制。主要发育夏子街扇、黄羊泉扇二大主扇体,夏子街扇细分为风南10、夏72、玛7三条支扇,西部的风南10支扇、东部的玛7支扇发育重力流(砂质碎屑流)沉积。夏72支扇位于玛北鼻状凸起上,鼻状凸起背景下发育的低缓沟槽控制着牵引流水系的展布。储层的成岩作用(压实、胶结)强度与沉积作用(泥杂基含量、粒度)关系密切,泥杂基含量、粒度为储层储集性能的主控因素。有利储集相带受沉积机制、沉积微相双重控制,重力流(砂质碎屑流)沉积整体物性最差;牵引流沉积视不同沉积相带,扇三角洲平原辫状河道、扇三角洲前缘远岸水下分流河道物性较差;扇三角洲前缘近岸水下分流河道、河口坝物性最优,优质储层主要分布在扇三角洲前缘近岸水下分流河道相带内。
- 玛北斜坡区 /
- 百口泉组 /
- 重矿物 /
- 地层倾角 /
- 古地貌 /
- 扇三角洲
Abstract: To clear the sedimentary characteristics of glutenite and the distribution of favourable accumulation facies, With the integrated study of core, logging, seismic and experimental analysis, this paper draw conclusions that the sedimentation in T₁b, Mabei Slope subordinate to fan delta deposition, including five sedimentary microfacies as follows:braided-stream channel in fan delta plain, sandy-debris flow in fan delta plain or fan delta front, nearshore underwater-distributary channel, offshore underwater-distributary channel, and estuary dam in fan delta front. There developed two mechanism named tractive current and gravity current, and mainly developed Xiazijie fan and Huangyangquan fan. Xiazijie fan is divided into three branch-fans named FN10, XIA72, MA7. FN10 branch-fan and MA7 branch-fan are mainly developed sandy-debris flow. XIA72 branch-fan locate in Mabei heave. The slow grooves developed in Mabei heave controlled the distribution of tractive current. The intensity of reservoir diagenesis(compaction and cementation) is closely related to deposition(matrix content and granularity). Matrix content and granularity are main controlling factor of accumulation property. Transportation mechanism and sedimentary microfacies controlled the distribution of favourable accumulation facies. Sandy-debris flow deposition is poor reservoir. The different sedimentary facies belt in tractive current have different accumulation property. Braided-stream channel in fan delta plain and offshore underwater-distributary channel are sub-poor reservoir. Nearshore underwater-distributary channel and estuary dam in fan delta front are the best reservoirs. High-quality reservoir are mainly located in nearshore underwater-distributary channel, and fan delta front.
- Mabei slope /
- T₁b /
- heavy mineral /
- dip angle /
- ancient landform /
- fan dalta

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[3]	单祥, 郭华军, 陈希光, 郭旭光, 佘敏, 李亚哲. 准噶尔盆地玛西斜坡区百口泉组砂砾岩埋藏溶蚀作用实验模拟研究 . 沉积学报, 2022, 40(5): 1406-1418. doi: 10.14027/j.issn.1000-0550.2021.050
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砂砾岩沉积特征分析及有利储集相带确定——以玛北斜坡区百口泉组为例

doi: 10.14027/j.cnki.cjxb.2015.06.016

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: <新疆大庆>科技攻关项目"玛北斜坡区百口泉组沉积相研究及储层精细描述"(编号:HX132-11311)资助

作者简介:
孟祥超男 1974年出生硕士高级工程师沉积储层 E-mail:mengxc_hz@petrochina.com.cn

收稿日期: 2014-07-04
修回日期: 2014-09-01
刊出日期: 2015-12-10

中图分类号: P618.13

关键词:

重矿物 /

古地貌 /

摘要: 为明确砂砾岩复杂储层的沉积特征及有利储集相带分布,通过岩心、测井、地震、实验分析等资料综合研究,认为玛北斜坡区百口泉组属近源快速堆积的扇三角洲沉积体系,主要发育扇三角洲平原辫状河道、扇三角洲平原/前缘砂质碎屑流、扇三角洲前缘近岸水下分流河道、远岸水下分流河道、河口坝五种主要沉积微相类型。发育牵引流、重力流两种搬运机制。主要发育夏子街扇、黄羊泉扇二大主扇体,夏子街扇细分为风南10、夏72、玛7三条支扇,西部的风南10支扇、东部的玛7支扇发育重力流(砂质碎屑流)沉积。夏72支扇位于玛北鼻状凸起上,鼻状凸起背景下发育的低缓沟槽控制着牵引流水系的展布。储层的成岩作用(压实、胶结)强度与沉积作用(泥杂基含量、粒度)关系密切,泥杂基含量、粒度为储层储集性能的主控因素。有利储集相带受沉积机制、沉积微相双重控制,重力流(砂质碎屑流)沉积整体物性最差;牵引流沉积视不同沉积相带,扇三角洲平原辫状河道、扇三角洲前缘远岸水下分流河道物性较差;扇三角洲前缘近岸水下分流河道、河口坝物性最优,优质储层主要分布在扇三角洲前缘近岸水下分流河道相带内。

English Abstract

Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T₁b, Mabei Slope, Junggar Basin

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

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

Received Date: 2014-07-04
Rev Recd Date: 2014-09-01
Publish Date: 2015-12-10

Keywords:

Abstract: To clear the sedimentary characteristics of glutenite and the distribution of favourable accumulation facies, With the integrated study of core, logging, seismic and experimental analysis, this paper draw conclusions that the sedimentation in T₁b, Mabei Slope subordinate to fan delta deposition, including five sedimentary microfacies as follows:braided-stream channel in fan delta plain, sandy-debris flow in fan delta plain or fan delta front, nearshore underwater-distributary channel, offshore underwater-distributary channel, and estuary dam in fan delta front. There developed two mechanism named tractive current and gravity current, and mainly developed Xiazijie fan and Huangyangquan fan. Xiazijie fan is divided into three branch-fans named FN10, XIA72, MA7. FN10 branch-fan and MA7 branch-fan are mainly developed sandy-debris flow. XIA72 branch-fan locate in Mabei heave. The slow grooves developed in Mabei heave controlled the distribution of tractive current. The intensity of reservoir diagenesis(compaction and cementation) is closely related to deposition(matrix content and granularity). Matrix content and granularity are main controlling factor of accumulation property. Transportation mechanism and sedimentary microfacies controlled the distribution of favourable accumulation facies. Sandy-debris flow deposition is poor reservoir. The different sedimentary facies belt in tractive current have different accumulation property. Braided-stream channel in fan delta plain and offshore underwater-distributary channel are sub-poor reservoir. Nearshore underwater-distributary channel and estuary dam in fan delta front are the best reservoirs. High-quality reservoir are mainly located in nearshore underwater-distributary channel, and fan delta front.

引用本文:

Citation:

MENG XiangChao, CHEN NengGui, WANG HaiMing, XU Yang, XIE ZongRui, ZOU ZhiWen, GUO HuaJun, LI YaZhe. Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T₁b, Mabei Slope, Junggar Basin[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1235-1246. doi: 10.14027/j.cnki.cjxb.2015.06.016

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砂砾岩沉积特征分析及有利储集相带确定——以玛北斜坡区百口泉组为例

doi: 10.14027/j.cnki.cjxb.2015.06.016

作者简介:
孟祥超男 1974年出生硕士高级工程师沉积储层 E-mail:mengxc_hz@petrochina.com.cn

计量

Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T₁b, Mabei Slope, Junggar Basin

计量

目录

砂砾岩沉积特征分析及有利储集相带确定——以玛北斜坡区百口泉组为例

doi: 10.14027/j.cnki.cjxb.2015.06.016

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年出生硕士高级工程师沉积储层 E-mail:mengxc_hz@petrochina.com.cn

English Abstract

Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T₁b, Mabei Slope, Junggar Basin

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

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

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砂砾岩沉积特征分析及有利储集相带确定——以玛北斜坡区百口泉组为例

doi: 10.14027/j.cnki.cjxb.2015.06.016

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

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Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T1b, Mabei Slope, Junggar Basin

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出版历程

目录

砂砾岩沉积特征分析及有利储集相带确定——以玛北斜坡区百口泉组为例

doi: 10.14027/j.cnki.cjxb.2015.06.016

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 硕士 高级工程师 沉积储层 E-mail:mengxc_hz@petrochina.com.cn

English Abstract

Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T1b, Mabei Slope, Junggar Basin

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

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作者简介:
孟祥超男 1974年出生硕士高级工程师沉积储层 E-mail:mengxc_hz@petrochina.com.cn

Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T₁b, Mabei Slope, Junggar Basin

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年出生硕士高级工程师沉积储层 E-mail:mengxc_hz@petrochina.com.cn

Sedimentary Characteristics of Glutenite and Its Favourable Accumulation Facies:A case study from T₁b, Mabei Slope, Junggar Basin

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

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