惠民凹陷孔店组末端扇沉积及其储层特征

张金亮

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

惠民凹陷孔店组末端扇沉积及其储层特征

张金亮

文章导航 > 沉积学报 > 2011 > 29(1): 1-13

张金亮. 惠民凹陷孔店组末端扇沉积及其储层特征[J]. 沉积学报, 2011, 29(1): 1-13.

引用本文:

张金亮. 惠民凹陷孔店组末端扇沉积及其储层特征[J]. 沉积学报, 2011, 29(1): 1-13.

ZHANG Jinliang. Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression[J]. Acta Sedimentologica Sinica, 2011, 29(1): 1-13.

Citation:

ZHANG Jinliang. Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression[J]. Acta Sedimentologica Sinica, 2011, 29(1): 1-13.

张金亮. 惠民凹陷孔店组末端扇沉积及其储层特征[J]. 沉积学报, 2011, 29(1): 1-13.

引用本文:

张金亮. 惠民凹陷孔店组末端扇沉积及其储层特征[J]. 沉积学报, 2011, 29(1): 1-13.

ZHANG Jinliang. Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression[J]. Acta Sedimentologica Sinica, 2011, 29(1): 1-13.

Citation:

ZHANG Jinliang. Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression[J]. Acta Sedimentologica Sinica, 2011, 29(1): 1-13.

惠民凹陷孔店组末端扇沉积及其储层特征

张金亮

中国海洋大学海洋地球科学学院山东青岛 266100

详细信息

通讯作者:
张金亮

计量

文章访问数: 2352
HTML全文浏览量: 2
PDF下载量: 1243
被引次数: 0

Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression

ZHANG Jinliang

College of Marine Geosciences, Ocean University of China, Qingdao Shandong 266100

More Information

Corresponding author: ZHANG Jinliang

摘要

摘要: 惠民凹陷孔店组为末端扇沉积，中部亚相是其沉积砂体的主体。根据岩芯观察并结合地震资料，将末端扇中部亚相划分为分流河道、河道漫溢和泥滩三种沉积微相。孔店组砂岩类型主要为中细粒的长石砂岩和岩屑长石砂岩。末端扇储层中发生了多种类型的成岩作用，主要的自生矿物包括黏土矿物、碳酸盐、石英和长石等。孔店组砂岩主要受到埋藏成岩作用的影响，成岩演化阶段正处于中成岩A期。孔店组末端扇储层性质受砂体微相和成岩作用的共同控制，发育绿泥石环边衬垫和塑性组分溶蚀成岩相的分流河道砂体的物性好于发育碳酸盐胶结和压实—充填成岩相的河道漫溢砂体。
- 末端扇 /
- 成岩作用 /
- 储层性质 /
- 成岩相
Abstract: Sedimentary facies of Kongdian sandstones is terminal fan. Middle zone is the main part of the tripartite terminal fan which can be divided into distributary channel, overbank and mudflat according to observation and description of cores combined with the numerous data of seismic. The sandstones type of Kongdian Formation are of finemedium grained arkose and lithic arkose. Terminal fan sandstone has undergone many types of diagenesis. Authigenic minerals in Kongdian reservoir include clay minerals, carbonate, quartz, feldspar and so on. Based on the study of burial history, the diagenetic stage of Kongdian Formation is in A period of mesodiagenesis. Reservoir quality of terminal fan in Kongdian Formation is mainly controlled by sandbody microfacies and diagenesis. Sedimentary microfacies resolves reservoir's original physical property, while diagenesis dominates final status of sandstone reservoir. There exists five diagenetic lithofacies in Kongdian sandstone, for example plastic composition dissolution lithofacies, chlorite gasket lithofacies, carbonate cementation lithofacies, compaction and filling lithofacies, quartz overgrowth lithofacies and so on. Diagenetic lithofacies is comprehensive reflection of diagenetic change and reservoir evolution of different microfacies sand. Distributary channel sandstone in connection with plastic composition dissolution or chlorite coating lithofacies is usually nice hydrocarbon pay bed, whereas overbank sandstone related with carbonate cementation or compaction and filling lithofacies is often low permeability layer. Terminal fan reservoir shows facies controlled feature.

- terminal fan /
- diagenesis /
- reservoir quality /
- diagenetic lithofacies

HTML全文

参考文献(0)

[1]	王乾右, 杨威, 葛云锦, 宋岩, 姜振学, 罗群, 左如斯, 李耀华, 刘聃, 张帆, 王耀华, 鲁健康. 不同沉积微相致密储层的成岩响应及其控储机理 . 沉积学报, 2021, 39(4): 841-862. doi: 10.14027/j.issn.1000-0550.2020.112
[2]	赵迪斐, 焦伟伟, 魏源, 张海杰, 李利格, 郭英海, Wang Geoff. 页岩储层成岩作用及其对储层脆性的影响 . 沉积学报, 2021, 39(4): 811-825. doi: 10.14027/j.issn.1000-0550.2021.034
[3]	张顺存, 黄立良, 冯右伦, 邹阳, 鲁新川, 郭晖. 准噶尔盆地玛北地区三叠系百口泉组储层成岩相特征 . 沉积学报, 2018, 36(2): 354-365. doi: 10.14027/j.issn.1000-0550.2018.030
[4]	冉冶, 王贵文, 赖锦, 周正龙, 崔玉峰, 代全齐, 陈晶, 王抒忱. 利用测井交会图法定量表征致密油储层成岩相——以鄂尔多斯盆地华池地区长7致密油储层为例 . 沉积学报, 2016, 34(4): 694-706. doi: 10.14027/j.cnki.cjxb.2016.04.010
[5]	牟传龙, 王秀平, 王启宇, 王远翀. 关于苏里格气田东二区盒8段储层成岩相的再认识 . 沉积学报, 2016, 34(2): 346-355. doi: 10.14027/j.cnki.cjxb.2016.02.013
[6]	张茜, 孙卫, 明红霞, 王倩, 张龙龙. 板桥-合水地区长6₃储层成岩相孔隙结构特征及优质储层分布 . 沉积学报, 2016, 34(2): 336-345. doi: 10.14027/j.cnki.cjxb.2016.02.012
[7]	曾小明, 于佳, 潘燕, 陈晓武, 张辉. 陵水凹陷北坡海底扇孔隙演化和成岩相研究 . 沉积学报, 2016, 34(6): 1198-1207. doi: 10.14027/j.cnki.cjxb.2016.06.017
[8]	王存武, 马东旭, 田兵, 梁建设, 王琪, 刘铁树. 鄂尔多斯盆地LX地区山西组储层成岩演化及成岩相研究 . 沉积学报, 2016, 34(3): 594-605. doi: 10.14027/j.cnki.cjxb.2016.03.017
[9]	郑庆华, 柳益群. 鄂尔多斯盆地镇北地区延长组长4+5致密油层成岩作用及成岩相 . 沉积学报, 2015, 33(5): 1000-1012. doi: 10.14027/j.cnki.cjxb.2015.05.016
[10]	. 白云凹陷珠江组深水扇成岩作用与成岩相分析 . 沉积学报, 2012, 30(3): 451-460.
[11]	罗忠. 层序界面对砂岩成岩作用及储层质量的影响——以鄂尔多斯盆地延河露头上三叠统延长组为例 . 沉积学报, 2007, 25(6): 903-914.
[12]	漆滨汶. 山东省牛庄洼陷古近系沙河街组沙三中亚段储集层成岩作用研究 . 沉积学报, 2007, 25(1): 99-109.
[13]	邱桂强. 东营凹陷古近系成岩层序特征与储集差异性分析 . 沉积学报, 2007, 25(6): 915-922.
[14]	李熙喆. 鄂尔多斯盆地上古生界层序格架内的成岩作用 . 沉积学报, 2007, 25(6): 923-933.
[15]	刘林玉, 王震亮, 张龙. 鄂尔多斯盆地镇北地区长3砂岩的成岩作用及其对储层的影响 . 沉积学报, 2006, (5): 690-697.
[16]	. 鄂尔多斯盆地镇北地区长3砂岩的成岩作用及其对储层的影响 . 沉积学报, 2006, 24(05): 690-697.
[17]	孟元林. 渤海湾盆地西部凹陷南段成岩相分析与优质储层预测 . 沉积学报, 2006, 24(2): 185-192.
[18]	张金亮, 司学强, 梁杰, 林辉. 陕甘宁盆地庆阳地区长8油层砂岩成岩作用及其对储层性质的影响 . 沉积学报, 2004, 22(2): 225-233.
[19]	王永标, 徐桂荣, 林启祥. 湖南慈利晚二叠世生物礁成岩作用及成岩相特征 . 沉积学报, 1998, 16(1): 132-136.
[20]	楼章华, 曾允孚. 扶杨油层孔隙水成因与砂岩成岩相研究 . 沉积学报, 1995, 13(S1): 63-70.

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: 2352
HTML全文浏览量: 2
PDF下载量: 1243
被引次数: 0

惠民凹陷孔店组末端扇沉积及其储层特征

张金亮

中国海洋大学海洋地球科学学院山东青岛 266100

通讯作者: 张金亮

收稿日期: 1900-01-01
修回日期: 1900-01-01
刊出日期: 2011-02-10

关键词:

末端扇 /

成岩作用 /

储层性质 /

成岩相

摘要: 惠民凹陷孔店组为末端扇沉积，中部亚相是其沉积砂体的主体。根据岩芯观察并结合地震资料，将末端扇中部亚相划分为分流河道、河道漫溢和泥滩三种沉积微相。孔店组砂岩类型主要为中细粒的长石砂岩和岩屑长石砂岩。末端扇储层中发生了多种类型的成岩作用，主要的自生矿物包括黏土矿物、碳酸盐、石英和长石等。孔店组砂岩主要受到埋藏成岩作用的影响，成岩演化阶段正处于中成岩A期。孔店组末端扇储层性质受砂体微相和成岩作用的共同控制，发育绿泥石环边衬垫和塑性组分溶蚀成岩相的分流河道砂体的物性好于发育碳酸盐胶结和压实—充填成岩相的河道漫溢砂体。

English Abstract

Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression

ZHANG Jinliang

College of Marine Geosciences, Ocean University of China, Qingdao Shandong 266100

Corresponding author: ZHANG Jinliang

Received Date: 1900-01-01
Rev Recd Date: 1900-01-01
Publish Date: 2011-02-10

Keywords:

Abstract: Sedimentary facies of Kongdian sandstones is terminal fan. Middle zone is the main part of the tripartite terminal fan which can be divided into distributary channel, overbank and mudflat according to observation and description of cores combined with the numerous data of seismic. The sandstones type of Kongdian Formation are of finemedium grained arkose and lithic arkose. Terminal fan sandstone has undergone many types of diagenesis. Authigenic minerals in Kongdian reservoir include clay minerals, carbonate, quartz, feldspar and so on. Based on the study of burial history, the diagenetic stage of Kongdian Formation is in A period of mesodiagenesis. Reservoir quality of terminal fan in Kongdian Formation is mainly controlled by sandbody microfacies and diagenesis. Sedimentary microfacies resolves reservoir's original physical property, while diagenesis dominates final status of sandstone reservoir. There exists five diagenetic lithofacies in Kongdian sandstone, for example plastic composition dissolution lithofacies, chlorite gasket lithofacies, carbonate cementation lithofacies, compaction and filling lithofacies, quartz overgrowth lithofacies and so on. Diagenetic lithofacies is comprehensive reflection of diagenetic change and reservoir evolution of different microfacies sand. Distributary channel sandstone in connection with plastic composition dissolution or chlorite coating lithofacies is usually nice hydrocarbon pay bed, whereas overbank sandstone related with carbonate cementation or compaction and filling lithofacies is often low permeability layer. Terminal fan reservoir shows facies controlled feature.


张金亮. 惠民凹陷孔店组末端扇沉积及其储层特征[J]. 沉积学报, 2011, 29(1): 1-13.

引用本文:

张金亮. 惠民凹陷孔店组末端扇沉积及其储层特征[J]. 沉积学报, 2011, 29(1): 1-13.

ZHANG Jinliang. Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression[J]. Acta Sedimentologica Sinica, 2011, 29(1): 1-13.

Citation:

ZHANG Jinliang. Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression[J]. Acta Sedimentologica Sinica, 2011, 29(1): 1-13.

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

惠民凹陷孔店组末端扇沉积及其储层特征

通讯作者:
张金亮

计量

Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression

Corresponding author: ZHANG Jinliang

计量

目录

惠民凹陷孔店组末端扇沉积及其储层特征

中国海洋大学海洋地球科学学院山东青岛 266100

通讯作者: 张金亮

English Abstract

Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression

College of Marine Geosciences, Ocean University of China, Qingdao Shandong 266100

Corresponding author: ZHANG Jinliang

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

惠民凹陷孔店组末端扇沉积及其储层特征

通讯作者: 张金亮

计量

出版历程

Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression

Corresponding author: ZHANG Jinliang

计量

出版历程

目录

惠民凹陷孔店组末端扇沉积及其储层特征

中国海洋大学海洋地球科学学院 山东青岛 266100

通讯作者: 张金亮

English Abstract

Deposition and Reservoir Characteristics of Terminal Fan in Kongdian Formation of Huimin Depression

College of Marine Geosciences, Ocean University of China, Qingdao Shandong 266100

Corresponding author: ZHANG Jinliang

全文HTML

目录

友情链接

期刊在线

联系我们

通讯作者:
张金亮

中国海洋大学海洋地球科学学院山东青岛 266100