三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式&mdash;&mdash;以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例

任双坡; 姚光庆; 毛文静

doi:10.14027/j.cnki.cjxb.2016.03.016

ISSN 1000-0550 CN 62-1038/P

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三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式——以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例

任双坡, 姚光庆, 毛文静

文章导航 > 沉积学报 > 2016 > 34(3): 582-593

任双坡, 姚光庆, 毛文静. 三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式——以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例[J]. 沉积学报, 2016, 34(3): 582-593. doi: 10.14027/j.cnki.cjxb.2016.03.016

引用本文:

REN ShuangPo, YAO GuangQing, MAO WenJing. Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield[J]. Acta Sedimentologica Sinica, 2016, 34(3): 582-593. doi: 10.14027/j.cnki.cjxb.2016.03.016

Citation:

REN ShuangPo, YAO GuangQing, MAO WenJing. Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield[J]. Acta Sedimentologica Sinica, 2016, 34(3): 582-593. doi: 10.14027/j.cnki.cjxb.2016.03.016

引用本文:

Citation:

REN ShuangPo, YAO GuangQing, MAO WenJing. Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield[J]. Acta Sedimentologica Sinica, 2016, 34(3): 582-593. doi: 10.14027/j.cnki.cjxb.2016.03.016

三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式——以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例

doi: 10.14027/j.cnki.cjxb.2016.03.016

任双坡^1,2,
姚光庆^1,2,,
毛文静^1,2

1.
中国地质大学构造与油气资源教育部重点实验室武汉 430074;
2.
中国地质大学资源学院武汉 430074

基金项目: 中国石油化工股份有限公司河南油田分公司重点项目(31350053-13-ZC0607-0005)

详细信息

作者简介:
任双坡,男,1989年出生,博士研究生,储层地质学,E-mail:rsp_123@126.com

通讯作者:
姚光庆,男,教授,E-mail:gqyao@cug.edu.cn

中图分类号: P618.13

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文章访问数: 1206
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Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield

1.
Key Laboratory of Tectonics and Petroleum Resource of the Ministry of Education, China University of Geosciences, Wuhan 430074, China;
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Funds: Key Project of Henan Oilfield, SINOPEC , No. 31350053-13-ZC0607-0005

摘要

摘要: 泌阳凹陷古城油田泌浅10区核三段广泛发育三角洲前缘水下分流河道薄层砂体。在储层精细沉积微相研究的基础上,综合应用岩芯、密井网测井等资料,对古城水下分流河道单砂体进行了精细刻画,建立了单砂体规模定量预测模型。依据河道规模将古城水下分流河道分为Ⅰ型、Ⅱ型、Ⅲ型河道3类。运用高分辨率层序地层学短期基准面旋回原理,对研究层段水下分流河道砂体成因类型进行了研究。结果表明,在基准面低幅上升且A/S<<1时,形成削截式水下分流河道砂体;A/S<1(接近1)时,形成完整式水下分流河道砂体。识别出单一河道砂体的叠置类型主要包括垂向叠置、侧向叠置、垂向相切、侧向相切、垂向分隔5种垂向叠置模式以及间湾相隔式、水平搭接式、侧向切叠式3种平面接触样式,并总结了各自的测井相识别标志。
- 泌浅10区 /
- 单砂体 /
- 短期基准面旋回 /
- 水下分流河道 /
- 三角洲前缘
Abstract: Thin sandbodies of subaqueous distributary channels of delta-front are widely developed in Biqian 10 area, Gucheng oil field, Biyang sag. Depending on fine study of reservoir sedimentary microfacies with integrating various data including cores and small well spacing logging data, we characterized the single sand body identification in compound subaqueous distributary channels and established a quantitative prediction model for single sand body scale, then we classified the subaqueous distributary channels into 3 types according to channel scale. Based on the short-term base-level cycle theory of high resolution sequence stratigraphy, the paper analyzes the genesis of subaqueous distributary channel sandstones in the study area. The result shows that in the course of base-level rising, A/S<<1, sandstone genetic type is mainly truncated distributary channel sandstone body, A/S<1(close to 1), sandstone genetic type is mainly integrated distributary channel sandstone body. We identified that there are five main vertical superimposition patterns of single sandbodies, including vertical superposition, lateral superposition, vertical tangency, lateral tangency and vertical separated, and three lateral contact patterns, including interdistributary contact, horizontal overlap contact and lateral superimposition-tangency contact, moreover, each type of logging-facies marks is summarized.
- Biqian 10 area /
- single sandbody /
- short-term base-level cycle /
- subaqueous distributary channel /
- delta-front

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[1]	李强强, 王喜鑫, 许月明, 薛婷, 李少华, 严春景. 湖平面变化对浅水三角洲前缘砂体构型的控制-来自数字露头的启示 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.055
[2]	赵军, 赵凯, 张金宇. 基于米氏旋回的三角洲前缘油层对比研究 . 沉积学报, 2022, 40(3): 801-812. doi: 10.14027/j.issn.1000-0550.2020.137
[3]	陈薪凯, 刘景彦, 陈程, 马骁. 主要构型要素细分下的曲流河单砂体识别 . 沉积学报, 2020, 38(1): 205-217. doi: 10.14027/j.issn.1000-0550.2019.011
[4]	秦润森, 岳红林, 周凤军, 吴穹螈, 雷源. 河控浅水三角洲前缘席状砂沉积特征及沉积模式探讨——以黄河口凹陷渤中34地区明下段为例 . 沉积学报, 2020, 38(2): 429-439. doi: 10.14027/j.issn.1000-0550.2019.027
[5]	厚刚福, 孙靖, 王力宝, 李亚哲, 李啸, 沈金龙, 窦洋, 陈扬, 韩守华. 不同古地貌单元水下分流河道沉积特征及其意义——以准噶尔盆地夏盐地区三工河组二段为例 . 沉积学报, 2019, 37(4): 825-833. doi: 10.14027/j.issn.1000-0550.2018.175
[6]	王俊, 赵家宏, 腾军, 王天煦, 鲍志东, 张红静, 袁淑琴, 林艳波, 高银山. 浅水三角洲前缘砂体地震沉积学研究——以松南乾安地区上白垩统青三段为例 . 沉积学报, 2018, 36(3): 570-583. doi: 10.14027/j.issn.1000-0550.2018.082
[7]	孙雨, 赵丹, 于利民, 王继平, 闫百泉, 马世忠. 浅水湖盆河控三角洲前缘砂体分布特征与沉积模式探讨——以松辽盆地北部永乐地区葡萄花油层为例 . 沉积学报, 2015, 33(3): 439-447. doi: 10.14027/j.cnki.cjxb.2015.03.002
[8]	杨友运, 何康宁, 任颖惠. 华庆地区长6₃储层内部建筑结构模式分析 . 沉积学报, 2015, 33(2): 357-363. doi: 10.14027/j.cnki.cjxb.2015.02.015
[9]	. 松辽盆地新立—新北地区嫩江组三段浅水三角洲水下分流河道砂体半定量解剖 . 沉积学报, 2012, 30(3): 511-521.
[10]	刘自亮. 三角洲前缘储集砂体的成因组合与分布规律——以松辽盆地大老爷府地区白垩系泉头组四段为例 . 沉积学报, 2009, 27(1): 32-40.
[11]	李玉兰. 松辽盆地南部月亮泡地区萨尔图油层Ⅰ砂组沉积微相研究及有利区带预测 . 沉积学报, 2008, 26(2): 265-270.
[12]	马世忠. 地下曲流河道单砂体内部薄夹层建筑结构研究方法 . 沉积学报, 2008, 26(4): 632-639.
[13]	张关龙. 三角洲前缘滑塌浊积体形成过程模拟 . 沉积学报, 2006, 24(1): 50-55.
[14]	王家豪, 姚光庆, 赵彦超. 浅水辫状河三角洲发育区短期基准面旋回划分及储层宏观特征分析 . 沉积学报, 2004, 22(1): 87-94.
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[16]	彭军, 郑荣才, 陈景山, 蔡勋育, 韦景春. 百色盆地那读组短期基准面旋回层序分析 . 沉积学报, 2002, 20(2): 203-209.
[17]	李凤杰, 王多云, 郑希民, 刘自亮, 王峰, 李树同, 王志坤. 陕甘宁盆地华池地区延长组缓坡带三角洲前缘的微相构成 . 沉积学报, 2002, 20(4): 582-587.
[18]	陈波, 陈恭洋, 保吉成. 港东油田二区一断块高分辨率层序地层 . 沉积学报, 2000, 18(2): 263-267,272.
[19]	楼章华, 卢庆梅, 蔡希源, 董百万, 张立庆. 湖平面升降对浅水三角洲前缘砂体形态的影响 . 沉积学报, 1998, 16(4): 27-31.
[20]	欧成华, 陈景山. 大芦家地区渐新统东二₁亚段三角洲前缘砂体微相及储集性研究 . 沉积学报, 1998, 16(4): 84-90.

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三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式——以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例

doi: 10.14027/j.cnki.cjxb.2016.03.016

1. 中国地质大学构造与油气资源教育部重点实验室武汉 430074;

2. 中国地质大学资源学院武汉 430074

基金项目: 中国石油化工股份有限公司河南油田分公司重点项目(31350053-13-ZC0607-0005)

作者简介:
任双坡,男,1989年出生,博士研究生,储层地质学,E-mail:rsp_123@126.com

通讯作者: 姚光庆,男,教授,E-mail:gqyao@cug.edu.cn

收稿日期: 2015-06-29
修回日期: 2015-09-12
刊出日期: 2016-06-10

中图分类号: P618.13

关键词:

泌浅10区 /

单砂体 /

短期基准面旋回 /

水下分流河道 /

三角洲前缘

摘要: 泌阳凹陷古城油田泌浅10区核三段广泛发育三角洲前缘水下分流河道薄层砂体。在储层精细沉积微相研究的基础上,综合应用岩芯、密井网测井等资料,对古城水下分流河道单砂体进行了精细刻画,建立了单砂体规模定量预测模型。依据河道规模将古城水下分流河道分为Ⅰ型、Ⅱ型、Ⅲ型河道3类。运用高分辨率层序地层学短期基准面旋回原理,对研究层段水下分流河道砂体成因类型进行了研究。结果表明,在基准面低幅上升且A/S<<1时,形成削截式水下分流河道砂体;A/S<1(接近1)时,形成完整式水下分流河道砂体。识别出单一河道砂体的叠置类型主要包括垂向叠置、侧向叠置、垂向相切、侧向相切、垂向分隔5种垂向叠置模式以及间湾相隔式、水平搭接式、侧向切叠式3种平面接触样式,并总结了各自的测井相识别标志。

English Abstract

Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield

1. Key Laboratory of Tectonics and Petroleum Resource of the Ministry of Education, China University of Geosciences, Wuhan 430074, China;

2. Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Funds: Key Project of Henan Oilfield, SINOPEC , No. 31350053-13-ZC0607-0005

Received Date: 2015-06-29
Rev Recd Date: 2015-09-12
Publish Date: 2016-06-10

Keywords:

Abstract: Thin sandbodies of subaqueous distributary channels of delta-front are widely developed in Biqian 10 area, Gucheng oil field, Biyang sag. Depending on fine study of reservoir sedimentary microfacies with integrating various data including cores and small well spacing logging data, we characterized the single sand body identification in compound subaqueous distributary channels and established a quantitative prediction model for single sand body scale, then we classified the subaqueous distributary channels into 3 types according to channel scale. Based on the short-term base-level cycle theory of high resolution sequence stratigraphy, the paper analyzes the genesis of subaqueous distributary channel sandstones in the study area. The result shows that in the course of base-level rising, A/S<<1, sandstone genetic type is mainly truncated distributary channel sandstone body, A/S<1(close to 1), sandstone genetic type is mainly integrated distributary channel sandstone body. We identified that there are five main vertical superimposition patterns of single sandbodies, including vertical superposition, lateral superposition, vertical tangency, lateral tangency and vertical separated, and three lateral contact patterns, including interdistributary contact, horizontal overlap contact and lateral superimposition-tangency contact, moreover, each type of logging-facies marks is summarized.

引用本文:

Citation:

REN ShuangPo, YAO GuangQing, MAO WenJing. Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield[J]. Acta Sedimentologica Sinica, 2016, 34(3): 582-593. doi: 10.14027/j.cnki.cjxb.2016.03.016

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三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式——以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例

doi: 10.14027/j.cnki.cjxb.2016.03.016

作者简介:
任双坡,男,1989年出生,博士研究生,储层地质学,E-mail:rsp_123@126.com

通讯作者:
姚光庆,男,教授,E-mail:gqyao@cug.edu.cn

计量

Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield

计量

目录

三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式——以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例

doi: 10.14027/j.cnki.cjxb.2016.03.016

1. 中国地质大学构造与油气资源教育部重点实验室武汉 430074;

2. 中国地质大学资源学院武汉 430074

作者简介:
任双坡,男,1989年出生,博士研究生,储层地质学,E-mail:rsp_123@126.com

通讯作者: 姚光庆,男,教授,E-mail:gqyao@cug.edu.cn

English Abstract

Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield

1. Key Laboratory of Tectonics and Petroleum Resource of the Ministry of Education, China University of Geosciences, Wuhan 430074, China;

2. Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

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三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式——以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例

doi: 10.14027/j.cnki.cjxb.2016.03.016

作者简介: 任双坡,男,1989年出生,博士研究生,储层地质学,E-mail:rsp_123@126.com

通讯作者: 姚光庆,男,教授,E-mail:gqyao@cug.edu.cn

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Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield

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三角洲前缘水下分流河道薄层单砂体成因类型及其叠置模式——以古城油田泌浅10区核三段Ⅳ-Ⅵ油组为例

doi: 10.14027/j.cnki.cjxb.2016.03.016

1. 中国地质大学构造与油气资源教育部重点实验室 武汉 430074; 2. 中国地质大学资源学院 武汉 430074

作者简介: 任双坡,男,1989年出生,博士研究生,储层地质学,E-mail:rsp_123@126.com

通讯作者: 姚光庆,男,教授,E-mail:gqyao@cug.edu.cn

English Abstract

Genetic Types and Superimposition Patterns of Subaqueous Distributary Channel Thin Sandbodies in Delta Front: A case study from the Ⅳ-Ⅵ reservoir groups of H3 in Biqian 10 area of Gucheng oilfield

1. Key Laboratory of Tectonics and Petroleum Resource of the Ministry of Education, China University of Geosciences, Wuhan 430074, China; 2. Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
任双坡,男,1989年出生,博士研究生,储层地质学,E-mail:rsp_123@126.com

通讯作者:
姚光庆,男,教授,E-mail:gqyao@cug.edu.cn

1. 中国地质大学构造与油气资源教育部重点实验室武汉 430074;

2. 中国地质大学资源学院武汉 430074

作者简介:
任双坡,男,1989年出生,博士研究生,储层地质学,E-mail:rsp_123@126.com

1. Key Laboratory of Tectonics and Petroleum Resource of the Ministry of Education, China University of Geosciences, Wuhan 430074, China;

2. Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China