埕岛油田沙三<sup>1</sup>段储层沉积学特征

周永红; 张晓宝; 王远坤; 吴茂炳

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埕岛油田沙三¹段储层沉积学特征

周永红, 张晓宝, 王远坤, 吴茂炳

文章导航 > 沉积学报 > 2000 > 18(2): 268-272

周永红, 张晓宝, 王远坤, 吴茂炳. 埕岛油田沙三1段储层沉积学特征[J]. 沉积学报, 2000, 18(2): 268-272.

引用本文:

周永红, 张晓宝, 王远坤, 吴茂炳. 埕岛油田沙三¹段储层沉积学特征[J]. 沉积学报, 2000, 18(2): 268-272.

ZHOU Youg hong, ZHANG Xiao bao, WANG Yuan kun, WU Mao bin. Characteristics of Reservoir Sedimentology in the Sha-3(1) Member of Chengdao Oilfield[J]. Acta Sedimentologica Sinica, 2000, 18(2): 268-272.

Citation:

ZHOU Youg hong, ZHANG Xiao bao, WANG Yuan kun, WU Mao bin. Characteristics of Reservoir Sedimentology in the Sha-3(1) Member of Chengdao Oilfield[J]. Acta Sedimentologica Sinica, 2000, 18(2): 268-272.

周永红, 张晓宝, 王远坤, 吴茂炳. 埕岛油田沙三1段储层沉积学特征[J]. 沉积学报, 2000, 18(2): 268-272.

引用本文:

周永红, 张晓宝, 王远坤, 吴茂炳. 埕岛油田沙三¹段储层沉积学特征[J]. 沉积学报, 2000, 18(2): 268-272.

Citation:

埕岛油田沙三¹段储层沉积学特征

1 胜利油田职工大学山东东营 257004;
2 中国科学院兰州地质研究所兰州 730000

详细信息

作者简介:
周永红,女,1967年出生,讲师,地质学

中图分类号: P618.130.2⁺¹

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文章访问数: 513
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Characteristics of Reservoir Sedimentology in the Sha-3(1) Member of Chengdao Oilfield

1 Staff University of Shengli Oilfield Dongying Shandong 257004;
2 Lanzhou Institute of Geology Chinese Academy of Sciences Lanzhou 730000

摘要

摘要: 沙三¹段是埕岛油田重要储集层之一,其储集层岩石学特征研究对该油田的滚动开发及勘探选区评价具有十分重要的指导意义。本文研究了沙三¹ 段储层沉积特征。研究认为 :⑴沙三¹ 段储集层为一套粗碎屑沉积岩,属河流 -滨浅湖沉积体系辫状河三角洲相,⑵块状层理粗砂岩相、槽状交错层理中细砂岩相、波状交错层理细砂岩相和平行层理细砂岩相为最有利的油气储集岩石相;Sf→Mm相组合、Sm→Mm相组合、St→Mm相组合以及Sr→Sh相组合是最发育的岩石相组合类型,也是最有利油气储集的岩石相组合,⑶物源方向主要为北东和西南;沉积相展布受构造控制,呈北北西 -南南东方向展布;沉积面貌具有西高东低、南高北低的沉积特征。
- 辫状河三角洲 /
- 储层沉积学 /
- 勘探选区评价 /
- 埕岛油田
Abstract: Based on the study of characterislies of reservoir petrology and sedimentology in target strata,the authors have put forward that the depositional environment of the Sha-3 member is river-shore shallow lake environment,the sedimentary sy stem belongs to lakeshore depositional system,and the sedimentary facies of the reservoir are braided river delta facies. The Sha-3(1) member is one of the most important reservoirs in Chengdao oilfiel d,sedimentary characteristics of which are very important for the rolling deve lopment and the evaluation of prospecting areas.The study concludes:(1) The rese rvoir of Sha-3(1) member is a set of coarse grain detrital sediment,belonging to river-shallow lake side depositional system with hraided river delta facies.(2) Massive gritstone,trough cross-stratification fine-middle sandstone,wave cross-s tratification fine sandstone and parallel-stratification fine sandstone are the most favourable petrofacies for petroleum accumilation;The combinations of Sf→M m,Sm→Mm,St→Mm and Sr→Sh are the most developed petrofacies combination type,and also the most favourable for petroleum accumulation.(3)The sedimentary der ivation is mainly northeast and southwest. The strelch of sedimentary facies,whi ch is under control of leetonics,goes north-northwest and south-southeast. The s edimentary province is geographically high in the west and low in the east,and high in the south and low in the north.
- braided river delta /
- reservoir sedimentology /
- evalu ation of prospecting area /
- Chengdao oilfield

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参考文献(2)

[1]	顾家裕等.沉积相与油气[M] .北京：石油工业出版社，1994
[2]	薛良清.扇三角洲、辫状河三角洲与三角洲体系的分类[J] .地质学报， 1991， 65(2)： 144～151

[1]	唐洪, 龙冠宇, 张章, 曲炳昌. 基于沉积数值模拟的砂质辫状河三角洲沉积特征与演化规律研究 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.088
[2]	彭旸, 王波, 于海跃, 董雨洋, 盛莉娜, 杨琳娜, 刘少治, 王少依, 朱晨. 新疆三塘湖盆地条湖-马朗凹陷中下侏罗纪沉积体系演化及物源分析 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2023.125
[3]	刘文锋, 张小栓, 刘瑾铭, 艾力曼·道尔吉null, 杨远峰. 玛湖凹陷西斜坡区三叠系白碱滩组沉积特征 . 沉积学报, 2022, 40(1): 192-202. doi: 10.14027/j.issn.1000-0550.2020.074
[4]	朱世发, 崔航, 陈嘉豪, 骆高俊, 王文禹, 杨祎, 施翌. 浅水三角洲沉积体系与储层岩石学特征 . 沉积学报, 2021, 39(1): 126-139. doi: 10.14027/j.issn.1000-0550.2020.115
[5]	倪仕琪, 宋继叶, 蔡煜琦, 张晓, 李真真, 邱余波, 张虎军, 蒋宏. 伊犁盆地南缘郎卡地区中侏罗统西山窑组沉积特征及演化 . 沉积学报, 2021, 39(2): 434-445. doi: 10.14027/j.issn.1000-0550.2020.003
[6]	赵晨帆, 于兴河, 付超, 韩小琴, 杜永慧. 曲流河三角洲—辫状河三角洲控制因素及演化过程探讨 . 沉积学报, 2019, 37(4): 768-784. doi: 10.14027/j.issn.1000-0550.2018.154
[7]	尹泽, 刘自亮, 彭楠, 沈芳, 谭梦琪, 王玉冲, 梁雨晨, 王红伟. 鄂尔多斯盆地西缘上三叠统延长组沉积相特征研究 . 沉积学报, 2019, 37(1): 163-176. doi: 10.14027/j.issn.1000-0550.2018.156
[8]	赵国祥, 官大勇, 刘朋波, 黄颖, 刘丹丹. 庙西南凸起馆陶组浅水辫状河三角洲沉积特征及砂体演化 . 沉积学报, 2018, 36(4): 807-817. doi: 10.14027/j.issn.1000-0550.2018.047
[9]	李小平, 柳保军, 丁琳, 郝建光, 龚文. 海相三角洲沉积单元划分及其对勘探砂体对比的意义——基于现代珠江三角洲沉积水动力综合研究 . 沉积学报, 2016, 34(3): 555-562. doi: 10.14027/j.cnki.cjxb.2016.03.013
[10]	黄薇, 吴海波, 李军辉, 刘赫. 海—塔盆地中部断陷带南屯组沉积体系配置及有利相带分析 . 沉积学报, 2016, 34(1): 120-128. doi: 10.14027/j.cnki.cjxb.2016.01.011
[11]	刘磊, 钟怡江, 陈洪德, 王峻. 中国东部箕状断陷湖盆扇三角洲与辫状河三角洲对比研究 . 沉积学报, 2015, 33(6): 1170-1181. doi: 10.14027/j.cnki.cjxb.2015.06.010
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[16]	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.
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埕岛油田沙三¹段储层沉积学特征

1 胜利油田职工大学山东东营 257004;

2 中国科学院兰州地质研究所兰州 730000

作者简介:
周永红,女,1967年出生,讲师,地质学

收稿日期: 1999-01-04
修回日期: 1999-03-09
刊出日期: 2000-06-10

中图分类号: P618.130.2⁺¹

关键词:

摘要: 沙三¹段是埕岛油田重要储集层之一,其储集层岩石学特征研究对该油田的滚动开发及勘探选区评价具有十分重要的指导意义。本文研究了沙三¹ 段储层沉积特征。研究认为 :⑴沙三¹ 段储集层为一套粗碎屑沉积岩,属河流 -滨浅湖沉积体系辫状河三角洲相,⑵块状层理粗砂岩相、槽状交错层理中细砂岩相、波状交错层理细砂岩相和平行层理细砂岩相为最有利的油气储集岩石相;Sf→Mm相组合、Sm→Mm相组合、St→Mm相组合以及Sr→Sh相组合是最发育的岩石相组合类型,也是最有利油气储集的岩石相组合,⑶物源方向主要为北东和西南;沉积相展布受构造控制,呈北北西 -南南东方向展布;沉积面貌具有西高东低、南高北低的沉积特征。

English Abstract

Characteristics of Reservoir Sedimentology in the Sha-3(1) Member of Chengdao Oilfield

1 Staff University of Shengli Oilfield Dongying Shandong 257004;

2 Lanzhou Institute of Geology Chinese Academy of Sciences Lanzhou 730000

Received Date: 1999-01-04
Rev Recd Date: 1999-03-09
Publish Date: 2000-06-10

Keywords:

Abstract: Based on the study of characterislies of reservoir petrology and sedimentology in target strata,the authors have put forward that the depositional environment of the Sha-3 member is river-shore shallow lake environment,the sedimentary sy stem belongs to lakeshore depositional system,and the sedimentary facies of the reservoir are braided river delta facies. The Sha-3(1) member is one of the most important reservoirs in Chengdao oilfiel d,sedimentary characteristics of which are very important for the rolling deve lopment and the evaluation of prospecting areas.The study concludes:(1) The rese rvoir of Sha-3(1) member is a set of coarse grain detrital sediment,belonging to river-shallow lake side depositional system with hraided river delta facies.(2) Massive gritstone,trough cross-stratification fine-middle sandstone,wave cross-s tratification fine sandstone and parallel-stratification fine sandstone are the most favourable petrofacies for petroleum accumilation;The combinations of Sf→M m,Sm→Mm,St→Mm and Sr→Sh are the most developed petrofacies combination type,and also the most favourable for petroleum accumulation.(3)The sedimentary der ivation is mainly northeast and southwest. The strelch of sedimentary facies,whi ch is under control of leetonics,goes north-northwest and south-southeast. The s edimentary province is geographically high in the west and low in the east,and high in the south and low in the north.

周永红, 张晓宝, 王远坤, 吴茂炳. 埕岛油田沙三1段储层沉积学特征[J]. 沉积学报, 2000, 18(2): 268-272.

引用本文:

周永红, 张晓宝, 王远坤, 吴茂炳. 埕岛油田沙三¹段储层沉积学特征[J]. 沉积学报, 2000, 18(2): 268-272.

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埕岛油田沙三¹段储层沉积学特征

作者简介:
周永红,女,1967年出生,讲师,地质学

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Characteristics of Reservoir Sedimentology in the Sha-3(1) Member of Chengdao Oilfield

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目录

埕岛油田沙三¹段储层沉积学特征

1 胜利油田职工大学山东东营 257004;

2 中国科学院兰州地质研究所兰州 730000

作者简介:
周永红,女,1967年出生,讲师,地质学

English Abstract

Characteristics of Reservoir Sedimentology in the Sha-3(1) Member of Chengdao Oilfield

1 Staff University of Shengli Oilfield Dongying Shandong 257004;

2 Lanzhou Institute of Geology Chinese Academy of Sciences Lanzhou 730000

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埕岛油田沙三1段储层沉积学特征

作者简介: 周永红,女,1967年出生,讲师,地质学

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Characteristics of Reservoir Sedimentology in the Sha-3(1) Member of Chengdao Oilfield

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埕岛油田沙三1段储层沉积学特征

1 胜利油田职工大学 山东东营 257004; 2 中国科学院兰州地质研究所 兰州 730000

作者简介: 周永红,女,1967年出生,讲师,地质学

English Abstract

Characteristics of Reservoir Sedimentology in the Sha-3(1) Member of Chengdao Oilfield

1 Staff University of Shengli Oilfield Dongying Shandong 257004; 2 Lanzhou Institute of Geology Chinese Academy of Sciences Lanzhou 730000

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埕岛油田沙三¹段储层沉积学特征

作者简介:
周永红,女,1967年出生,讲师,地质学

埕岛油田沙三¹段储层沉积学特征

1 胜利油田职工大学山东东营 257004;

2 中国科学院兰州地质研究所兰州 730000

作者简介:
周永红,女,1967年出生,讲师,地质学

1 Staff University of Shengli Oilfield Dongying Shandong 257004;

2 Lanzhou Institute of Geology Chinese Academy of Sciences Lanzhou 730000