博格达山周缘中二叠统芦草沟组与红雁池组沉积特征及演化

王越; 林会喜; 张奎华; 张关龙; 汪誉新; 白仲才

doi:10.14027/j.issn.1000-0550.2018.039

ISSN 1000-0550 CN 62-1038/P

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博格达山周缘中二叠统芦草沟组与红雁池组沉积特征及演化

王越, 林会喜, 张奎华, 张关龙, 汪誉新, 白仲才

文章导航 > 沉积学报 > 2018 > 36(3): 500-509

王越, 林会喜, 张奎华, 张关龙, 汪誉新, 白仲才. 博格达山周缘中二叠统芦草沟组与红雁池组沉积特征及演化[J]. 沉积学报, 2018, 36(3): 500-509. doi: 10.14027/j.issn.1000-0550.2018.039

引用本文:

WANG Yue, LIN HuiXi, ZHANG KuiHua, ZHANG GuanLong, WANG YuXin, BAI ZhongCai. Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain[J]. Acta Sedimentologica Sinica, 2018, 36(3): 500-509. doi: 10.14027/j.issn.1000-0550.2018.039

Citation:

WANG Yue, LIN HuiXi, ZHANG KuiHua, ZHANG GuanLong, WANG YuXin, BAI ZhongCai. Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain[J]. Acta Sedimentologica Sinica, 2018, 36(3): 500-509. doi: 10.14027/j.issn.1000-0550.2018.039

引用本文:

Citation:

WANG Yue, LIN HuiXi, ZHANG KuiHua, ZHANG GuanLong, WANG YuXin, BAI ZhongCai. Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain[J]. Acta Sedimentologica Sinica, 2018, 36(3): 500-509. doi: 10.14027/j.issn.1000-0550.2018.039

博格达山周缘中二叠统芦草沟组与红雁池组沉积特征及演化

doi: 10.14027/j.issn.1000-0550.2018.039

1.
胜利石油管理局博士后科研工作站, 山东东营 257000;
2.
中国石化胜利油田分公司勘探开发研究院, 山东东营 257015

基金项目: 胜利石油管理局博士后科研课题"准东南地区二叠系沉积充填演化及储层发育模式研究"资助

详细信息

作者简介:
王越,男,1988年出生,博士后,沉积学及层序地层学,E-mail:620788364@qq.com

中图分类号: P512.2

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文章访问数: 426
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PDF下载量: 383
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Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain

1.
Post-doctoral Research Station, Shengli Oilfield Company, Dongying, Shandong 257000, China;
2.
Research Institute of Petroleum Exploration and Development, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257015, China

Funds: Post-Doctoral Research Station, Shengli Oilfield Company:Study on Sedimentary Filling Evolution and Reservoir Development Model of Permian in the Southeast of Junggar Basin

摘要

摘要: 通过对博格达山周缘典型露头剖面的芦草沟组与红雁池组进行详细观察和精细测量，结合柴窝堡凹陷内的钻测井、岩芯资料，详细分析了该区的地层特征、沉积相类型及分布特征，进一步探讨了芦草沟组和红雁池的沉积演化过程。研究结果表明：芦草沟组与红雁池组自下而上均可划分为一段、二段和三段，两个组的地层在柴窝堡凹陷内保留相对完整，而在博格达山山前剥蚀较严重，不同地区残留厚度不一；芦草沟组至红雁池组为一个湖侵到湖退的沉积过程，芦草沟组一段、二段主要发育近岸水下扇中扇和外扇，芦草沟组三段以半深湖-深湖沉积为主，红雁池组一段、二段以扇三角洲前缘、滩坝和滨浅湖沉积为主，红雁池组三段主要发育扇三角洲平原。
- 博格达山 /
- 芦草沟组 /
- 红雁池组 /
- 地层特征 /
- 沉积相 /
- 沉积演化
Abstract: Through detailed outcrop observation and measurement of the Lucaogou and Hongyanchi Formations on the periphery of the Bogda Mountain, combined with drilling, well-logging and core data from the Chaiwobao depression, the stratigraphic characteristics, sedimentary facies types, and their distribution characteristics were deeply analyzed, furthermore, evolution process of the Lucaogou and Hongyanchi Formations were also discussed in this paper. The results showed that the Lucaogou and Hongyanchi Formations could be both divided into three members, the first through the third from the bottom up, which were kept relatively complete in the Chaiwogou depression whereas the residual thickness were varied in different areas in front of the Bogda Mountain with serious erossion. The sedimentary process of the Lucaogou formation to Hongyanchi Formation was from a lake transgression to a lake regression. The first and second members of Lucaogou Formation were mainly developed in a nearshore subaqueous middle fan and outer fan; the third member of Lucaogou Formation was widely developed in a semi-deep and deep lake. The first and second members of Hongyanchi Formation were mainly developed in fan delta front, sand bar and beach, and shore shallow lake whereas the third member was mainly developed in a fan delta plain.
- Bogda Mountain /
- Lucaogou Formation /
- Hongyanchi Formation /
- stratigraphic characteristics /
- sedimentary facies /
- sedimentary evolution

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[1]	王纪煊, 胡忠贵, 远光辉, 李世临, 张俊, 王文静, 张宸瑜. 碳酸盐岩-蒸发岩共生体系沉积特征及演化模式——以四川盆地东部高台组为例 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.024
[2]	潘进, 刘新龙, 李辉, 刘超威, 李树博, 陈洪, 王泽胜, 李宗浩, 金腾瑞, 陈美玲, 朱新亭, 樊向东. 阜东斜坡芦草沟组岩相组合特征及展布规律 . 沉积学报, 2023, 41(5): 1366-1379. doi: 10.14027/j.issn.1000-0550.2022.133
[3]	邓孝亮, 张迎朝, 陆江, 甘军, 詹冶萍, 刘凯. 文昌B凹陷北坡珠海组潮汐沉积特征及演化 . 沉积学报, 2020, 38(6): 1313-1326. doi: 10.14027/j.issn.1000-0550.2020.007
[4]	李哲萱, 柳益群, 周鼎武, 焦鑫, 南云. 三塘湖盆地二叠系芦草沟组喷爆岩岩石学、矿物学特征及相关问题探讨 . 沉积学报, 2019, 37(3): 455-465. doi: 10.14027/j.issn.1000-0550.2018.145
[5]	王越, 张关龙, 王圣柱, 林会喜, 张奎华, 汪誉新, 曲彦胜, 张顺, 张亚男. 博格达山东北缘上二叠统沉积特征与沉积演化模式 . 沉积学报, 2019, 37(3): 579-588. doi: 10.14027/j.issn.1000-0550.2018.159
[6]	侯中帅, 陈世悦, 郭宇鑫, 王志金, 赫庆庆, 崔绮梦. 华北中南部博山地区上古生界沉积相与沉积演化特征 . 沉积学报, 2018, 36(4): 731-742. doi: 10.14027/j.issn.1000-0550.2018.052
[7]	胡双全, 杜贵超, 甄胜利. 泰国呵叻盆地二叠系Pha Nok Khao组碳酸盐岩沉积相特征 . 沉积学报, 2017, 35(4): 789-796. doi: 10.14027/j.cnki.cjxb.2017.04.013
[8]	张亚奇, 马世忠, 高阳, 李映艳, 张景, 王黎, 孙雨, 许方哲, 李杭. 吉木萨尔凹陷芦草沟组致密油储层沉积相分析 . 沉积学报, 2017, 35(2): 358-370. doi: 10.14027/j.cnki.cjxb.2017.02.013
[9]	王越, 陈世悦, 梁绘媛, 王剑, 李天宝. 鄂尔多斯盆地保德地区上古生界沉积相与沉积演化特征 . 沉积学报, 2016, 34(4): 775-784. doi: 10.14027/j.cnki.cjxb.2016.04.017
[10]	郑有伟, 王亚东, 郭建明, 刘兴旺, 赵光亮, 苏龙, 郑建京. 准噶尔盆地东南缘侏罗系重矿物演化特征及对博格达山隆升的响应 . 沉积学报, 2016, 34(6): 1147-1154. doi: 10.14027/j.cnki.cjxb.2016.06.012
[11]	汤建荣, 王金友, 章诚诚, 宋广增, 石英涛, 张雷. 致密气源层内沉积特征及与致密砂岩气藏关系——以川东北元坝地区须三段为例 . 沉积学报, 2015, 33(6): 1224-1234. doi: 10.14027/j.cnki.cjxb.2015.06.015
[12]	王改云, 刘金萍, 王后金, 简晓玲, 杜民. 北黄海盆地东部坳陷中生界沉积特征及演化 . 沉积学报, 2015, 33(3): 561-567. doi: 10.14027/j.cnki.cjxb.2015.03.014
[13]	. 鹤庆—松桂地区上三叠统中窝组含矿岩系沉积相特征及演化 . 沉积学报, 2014, 32(4): 623-633.
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[20]	吴少波. 博格达山前凹陷上二叠统乌拉泊组沉积相及沉积模式 . 沉积学报, 2001, 19(3): 333-339.

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博格达山周缘中二叠统芦草沟组与红雁池组沉积特征及演化

doi: 10.14027/j.issn.1000-0550.2018.039

1. 胜利石油管理局博士后科研工作站, 山东东营 257000;

2. 中国石化胜利油田分公司勘探开发研究院, 山东东营 257015

基金项目: 胜利石油管理局博士后科研课题"准东南地区二叠系沉积充填演化及储层发育模式研究"资助

作者简介:
王越,男,1988年出生,博士后,沉积学及层序地层学,E-mail:620788364@qq.com

收稿日期: 2017-04-13
修回日期: 2017-08-01
刊出日期: 2018-06-10

中图分类号: P512.2

关键词:

沉积相 /

摘要: 通过对博格达山周缘典型露头剖面的芦草沟组与红雁池组进行详细观察和精细测量，结合柴窝堡凹陷内的钻测井、岩芯资料，详细分析了该区的地层特征、沉积相类型及分布特征，进一步探讨了芦草沟组和红雁池的沉积演化过程。研究结果表明：芦草沟组与红雁池组自下而上均可划分为一段、二段和三段，两个组的地层在柴窝堡凹陷内保留相对完整，而在博格达山山前剥蚀较严重，不同地区残留厚度不一；芦草沟组至红雁池组为一个湖侵到湖退的沉积过程，芦草沟组一段、二段主要发育近岸水下扇中扇和外扇，芦草沟组三段以半深湖-深湖沉积为主，红雁池组一段、二段以扇三角洲前缘、滩坝和滨浅湖沉积为主，红雁池组三段主要发育扇三角洲平原。

English Abstract

Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain

1. Post-doctoral Research Station, Shengli Oilfield Company, Dongying, Shandong 257000, China;

2. Research Institute of Petroleum Exploration and Development, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257015, China

Funds: Post-Doctoral Research Station, Shengli Oilfield Company:Study on Sedimentary Filling Evolution and Reservoir Development Model of Permian in the Southeast of Junggar Basin

Received Date: 2017-04-13
Rev Recd Date: 2017-08-01
Publish Date: 2018-06-10

Keywords:

Abstract: Through detailed outcrop observation and measurement of the Lucaogou and Hongyanchi Formations on the periphery of the Bogda Mountain, combined with drilling, well-logging and core data from the Chaiwobao depression, the stratigraphic characteristics, sedimentary facies types, and their distribution characteristics were deeply analyzed, furthermore, evolution process of the Lucaogou and Hongyanchi Formations were also discussed in this paper. The results showed that the Lucaogou and Hongyanchi Formations could be both divided into three members, the first through the third from the bottom up, which were kept relatively complete in the Chaiwogou depression whereas the residual thickness were varied in different areas in front of the Bogda Mountain with serious erossion. The sedimentary process of the Lucaogou formation to Hongyanchi Formation was from a lake transgression to a lake regression. The first and second members of Lucaogou Formation were mainly developed in a nearshore subaqueous middle fan and outer fan; the third member of Lucaogou Formation was widely developed in a semi-deep and deep lake. The first and second members of Hongyanchi Formation were mainly developed in fan delta front, sand bar and beach, and shore shallow lake whereas the third member was mainly developed in a fan delta plain.

引用本文:

Citation:

WANG Yue, LIN HuiXi, ZHANG KuiHua, ZHANG GuanLong, WANG YuXin, BAI ZhongCai. Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain[J]. Acta Sedimentologica Sinica, 2018, 36(3): 500-509. doi: 10.14027/j.issn.1000-0550.2018.039

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博格达山周缘中二叠统芦草沟组与红雁池组沉积特征及演化

doi: 10.14027/j.issn.1000-0550.2018.039

作者简介:
王越,男,1988年出生,博士后,沉积学及层序地层学,E-mail:620788364@qq.com

计量

Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain

计量

目录

博格达山周缘中二叠统芦草沟组与红雁池组沉积特征及演化

doi: 10.14027/j.issn.1000-0550.2018.039

1. 胜利石油管理局博士后科研工作站, 山东东营 257000;

2. 中国石化胜利油田分公司勘探开发研究院, 山东东营 257015

作者简介:
王越,男,1988年出生,博士后,沉积学及层序地层学,E-mail:620788364@qq.com

English Abstract

Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain

1. Post-doctoral Research Station, Shengli Oilfield Company, Dongying, Shandong 257000, China;

2. Research Institute of Petroleum Exploration and Development, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257015, China

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博格达山周缘中二叠统芦草沟组与红雁池组沉积特征及演化

doi: 10.14027/j.issn.1000-0550.2018.039

作者简介: 王越,男,1988年出生,博士后,沉积学及层序地层学,E-mail:620788364@qq.com

计量

出版历程

Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain

计量

出版历程

目录

博格达山周缘中二叠统芦草沟组与红雁池组沉积特征及演化

doi: 10.14027/j.issn.1000-0550.2018.039

1. 胜利石油管理局博士后科研工作站, 山东东营 257000; 2. 中国石化胜利油田分公司勘探开发研究院, 山东东营 257015

作者简介: 王越,男,1988年出生,博士后,沉积学及层序地层学,E-mail:620788364@qq.com

English Abstract

Sedimentary Characteristics and Evolution of the Middle Permain Lucaogou Formation and Hongyanchi Formation on the Periphery of Bogda Mountain

1. Post-doctoral Research Station, Shengli Oilfield Company, Dongying, Shandong 257000, China; 2. Research Institute of Petroleum Exploration and Development, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257015, China

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
王越,男,1988年出生,博士后,沉积学及层序地层学,E-mail:620788364@qq.com

1. 胜利石油管理局博士后科研工作站, 山东东营 257000;

2. 中国石化胜利油田分公司勘探开发研究院, 山东东营 257015

作者简介:
王越,男,1988年出生,博士后,沉积学及层序地层学,E-mail:620788364@qq.com

1. Post-doctoral Research Station, Shengli Oilfield Company, Dongying, Shandong 257000, China;

2. Research Institute of Petroleum Exploration and Development, Shengli Oilfield Company, SINOPEC, Dongying, Shandong 257015, China