物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用

贺静

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

物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用

贺静

文章导航 > 沉积学报 > 2011 > 29(1): 80-87

贺静. 物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用[J]. 沉积学报, 2011, 29(1): 80-87.

引用本文:

贺静. 物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用[J]. 沉积学报, 2011, 29(1): 80-87.

HE Jing. Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin[J]. Acta Sedimentologica Sinica, 2011, 29(1): 80-87.

Citation:

HE Jing. Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin[J]. Acta Sedimentologica Sinica, 2011, 29(1): 80-87.

贺静. 物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用[J]. 沉积学报, 2011, 29(1): 80-87.

引用本文:

贺静. 物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用[J]. 沉积学报, 2011, 29(1): 80-87.

HE Jing. Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin[J]. Acta Sedimentologica Sinica, 2011, 29(1): 80-87.

Citation:

HE Jing. Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin[J]. Acta Sedimentologica Sinica, 2011, 29(1): 80-87.

物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用

贺静

长庆油田分公司勘探开发研究院西安 710018

详细信息

通讯作者:
贺静

计量

文章访问数: 2483
HTML全文浏览量: 3
PDF下载量: 911
被引次数: 0

Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin

HE Jing

Research Institute of Exploration and Development of Changqing Oilfield Company,PetroChina,Xi'an710018;

More Information

Corresponding author: HE Jing

摘要

摘要: 延长组长6油层组是鄂尔多斯盆地主力产油层，平面上储层储集性能差异较大。通过盆地中部大量长6砂岩岩矿资料，结合盆地周缘露头剖面资料系统分析，认为鄂尔多斯盆地中部长6沉积期存在西部、北东、西北、北部、东南方向及多物源控制的沉积区，且受不同方向物源控制的长6砂岩轻、重矿物组合，填隙物类型和组合及成岩矿物等均不相同，其中混源区受多物源的共同影响，但轻、重矿物组合及孔隙发育程度主要受主物源控制；砂岩成熟度、粒径、碎屑组分、填隙物类型与组合和成岩作用是控制长6砂岩储层孔隙发育的主要因素，且不同物源控制区长6储集砂岩的孔隙保存条件不同，物性相差较大。研究结果说明确定不同方向物源控制区、混源沉积区长6储集砂岩孔隙特征及孔隙发育控制因素是掌握孔隙性砂体分布规律的前提。
- 鄂尔多斯盆地 /
- 物源 /
- 延长组长6 /
- 孔隙
Abstract: Chang6 reservoir is the leading pay formation of the Yanchang Formation in the center of Ordos basin, but reservoir quality of genetic sandbodies shows a big difference in horizontal. By studying the light and heavy mineral combination characteristics of chang6 reservoir sandstone and typical outcrops, it is believed that there exist five main source directions of the west, northeast, northwest, north and southeast in the depositional period of chang6 oilbed of Yangchang Formation in the center of Ordos basin. The characteristics of the light and heavy mineral combination, interstitial matrix and diagenetic mineral of chang6 reservoir sandstone controlled by different source directions were different. In addition, there exist some mixed sources areas which were converged by the west, northeast, northwest, north and southeast sources. The characteristics of light and heavy mineral combination, interstitial matrix, diagenetic mineral and porosity of its reservoir were affected by the main source. The controlling factors of the sandstone reservoir porosity development of Chang 6 include the sandstone maturity, grain size, detritus composition, interstitial matrix and diagenesis. The reservoir porosity is closely related to the various provenances. As a result, porosity distribution is predictable.
- Ordos basin /
- provenances /
- Chang6 oilbed of Yangchang Formation /
- porosity

HTML全文

参考文献(0)

[1]	郑庆华, 刘行军, 张荣莉, 王克, 王自亮. 页岩油岩石类型组合及储集能力定量研究新方法——以鄂尔多斯盆地陇东地区延长组长7油层组为例 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.078
[2]	张云望, 金鑫, 乔培军, 李滨兵, 洪彦哲, 陈俞超, 芦刚, 杜怡星, 时志强. 鄂尔多斯盆地东北部下侏罗统富县组沉积物源分析 . 沉积学报, 2023, 41(5): 1414-1429. doi: 10.14027/j.issn.1000-0550.2022.154
[3]	郑庆华, 刘行军, 柳益群, 周鼎武, 杨开艳, 王贵文, 张洋洋, 陈朕, 刘亮. 鄂尔多斯盆地延长组长7油层组碳酸质喷积岩初探 . 沉积学报, 2021, 39(5): 1222-1238. doi: 10.14027/j.issn.1000-0550.2020.075
[4]	贾浪波, 钟大康, 孙海涛, 严锐涛, 张春林, 莫午零, 邱存, 董媛, 李兵, 廖广新. 鄂尔多斯盆地本溪组沉积物物源探讨及其构造意义 . 沉积学报, 2019, 37(5): 1087-1103. doi: 10.14027/j.issn.1000-0550.2019.014
[5]	曹江骏, 杨友运, 陈朝兵, 卜广平, 王茜, 杨一茗. 致密砂岩储层骨架砂体构型特征——以鄂尔多斯盆地合水地区延长组长6段砂体为例 . 沉积学报, 2019, 37(6): 1105-1116. doi: 10.14027/j.issn.1000-0550.2019.051
[6]	刘福田, 李荣西, 刘新社, 杨鸣一, 赵帮胜, 吴小力, 覃小丽. 鄂尔多斯盆地苏里格西部气田“源控”主导的天然气成藏研究 . 沉积学报, 2019, 37(6): 1129-1139. doi: 10.14027/j.issn.1000-0550.2019.052
[7]	胡鹏, 于兴河, 陈宏亮, 赵晨帆, 周进松, 韩小琴, 李亚龙. 障壁坝砂体储层特征与成岩孔隙定量演化模式——以鄂尔多斯盆地延长探区本溪组为例 . 沉积学报, 2019, 37(2): 390-402. doi: 10.14027/j.issn.1000-0550.2018.121
[8]	石鑫, 侯明才, 黄虎, 胡小龙, 江文剑, 吴斌, 缪宗利, 郑斯赫. 伊犁盆地南缘中-下侏罗统物源分析及其对南天山造山带演化的启示 . 沉积学报, 2018, 36(3): 446-455. doi: 10.14027/j.issn.1000-0550.2018.115
[9]	梁飞, 黄文辉, 牛君. 鄂尔多斯盆地西南缘二叠系山西组山1段-下石盒子组盒8段物源分析 . 沉积学报, 2018, 36(1): 142-153. doi: 10.3969/j.issn.1000-0550.2018.016
[10]	李亚龙, 于兴河, 周进松, 单新, 韩小琴, 史新, 胡鹏. 鄂尔多斯盆地东南部山2段物源与曲流河三角洲沉积体系 . 沉积学报, 2017, 35(3): 540-551. doi: 10.14027/j.cnki.cjxb.2017.03.012
[11]	. 贺兰山地区中奥陶统樱桃沟组物源及构造背景分析 . 沉积学报, 2014, 32(2): 205-217.
[12]	. 鄂尔多斯盆地乌审旗地区上古生界砂岩碎屑锆石U-Pb年龄及其地质意义 . 沉积学报, 2014, 32(4): 643-653.
[13]	. 鄂尔多斯盆地延长组长8油层组石油成藏机理及成藏模式 . 沉积学报, 2013, 31(04): 683-692.
[14]	. 鄂尔多斯盆地延长组长9砂体的垂向结构及主控因素分析 . 沉积学报, 2013, 31(1): 77-88.
[15]	. 鄂尔多斯盆地吴堡地区上三叠统延长组原油地球化学特征及油源对比 . 沉积学报, 2013, 31(2): 374-383.
[16]	. 鄂尔多斯盆地延长组长10期沉积环境与沉积体系 . 沉积学报, 2011, 29(6): 1105-1114.
[17]	郭彦如刘化清李相博完颜容郑希民. 大型坳陷湖盆层序地层格架的研究方法体系 ———以鄂尔多斯盆地中生界延长组为例 . 沉积学报, 2008, 26(3): 384-391.
[18]	赵俊兴. 鄂尔多斯盆地南部延长组长6时期物源状况分析 . 沉积学报, 2008, 26(4): 610-616.
[19]	刘化清, 廖建波, 房乃珍, 林卫东, 程玉红, 王宏波, 冯明. 鄂尔多斯盆地环县地区长6沉积体系展布特征 . 沉积学报, 2005, 23(4): 584-588.
[20]	张绍平. 鄂尔多斯盆地中部奥陶系顶盐溶作用及其储集孔隙成因 . 沉积学报, 1994, 12(1): 72-80.

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: 2483
HTML全文浏览量: 3
PDF下载量: 911
被引次数: 0

物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用

贺静

长庆油田分公司勘探开发研究院西安 710018

通讯作者: 贺静

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

关键词:

鄂尔多斯盆地 /

物源 /

延长组长6 /

孔隙

摘要: 延长组长6油层组是鄂尔多斯盆地主力产油层，平面上储层储集性能差异较大。通过盆地中部大量长6砂岩岩矿资料，结合盆地周缘露头剖面资料系统分析，认为鄂尔多斯盆地中部长6沉积期存在西部、北东、西北、北部、东南方向及多物源控制的沉积区，且受不同方向物源控制的长6砂岩轻、重矿物组合，填隙物类型和组合及成岩矿物等均不相同，其中混源区受多物源的共同影响，但轻、重矿物组合及孔隙发育程度主要受主物源控制；砂岩成熟度、粒径、碎屑组分、填隙物类型与组合和成岩作用是控制长6砂岩储层孔隙发育的主要因素，且不同物源控制区长6储集砂岩的孔隙保存条件不同，物性相差较大。研究结果说明确定不同方向物源控制区、混源沉积区长6储集砂岩孔隙特征及孔隙发育控制因素是掌握孔隙性砂体分布规律的前提。

English Abstract

Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin

HE Jing

Research Institute of Exploration and Development of Changqing Oilfield Company,PetroChina,Xi'an710018;

Corresponding author: HE Jing

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

Keywords:

Ordos basin /
provenances /
Chang6 oilbed of Yangchang Formation /
porosity

Abstract: Chang6 reservoir is the leading pay formation of the Yanchang Formation in the center of Ordos basin, but reservoir quality of genetic sandbodies shows a big difference in horizontal. By studying the light and heavy mineral combination characteristics of chang6 reservoir sandstone and typical outcrops, it is believed that there exist five main source directions of the west, northeast, northwest, north and southeast in the depositional period of chang6 oilbed of Yangchang Formation in the center of Ordos basin. The characteristics of the light and heavy mineral combination, interstitial matrix and diagenetic mineral of chang6 reservoir sandstone controlled by different source directions were different. In addition, there exist some mixed sources areas which were converged by the west, northeast, northwest, north and southeast sources. The characteristics of light and heavy mineral combination, interstitial matrix, diagenetic mineral and porosity of its reservoir were affected by the main source. The controlling factors of the sandstone reservoir porosity development of Chang 6 include the sandstone maturity, grain size, detritus composition, interstitial matrix and diagenesis. The reservoir porosity is closely related to the various provenances. As a result, porosity distribution is predictable.

贺静. 物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用[J]. 沉积学报, 2011, 29(1): 80-87.

引用本文:

贺静. 物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用[J]. 沉积学报, 2011, 29(1): 80-87.

HE Jing. Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin[J]. Acta Sedimentologica Sinica, 2011, 29(1): 80-87.

Citation:

HE Jing. Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin[J]. Acta Sedimentologica Sinica, 2011, 29(1): 80-87.

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

物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用

通讯作者:
贺静

计量

Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin

Corresponding author: HE Jing

计量

目录

物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用

长庆油田分公司勘探开发研究院西安 710018

通讯作者: 贺静

English Abstract

Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin

Research Institute of Exploration and Development of Changqing Oilfield Company,PetroChina,Xi'an710018;

Corresponding author: HE Jing

全文HTML

目录

友情链接

期刊在线

联系我们

留言板

物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用

通讯作者: 贺静

计量

出版历程

Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin

Corresponding author: HE Jing

计量

出版历程

目录

物源对鄂尔多斯盆地中部延长组x长6砂岩孔隙发育的控制作用

长庆油田分公司勘探开发研究院西安 710018

通讯作者: 贺静

English Abstract

Effects of Provenance on Porosity Development of Chang 6 Sandstone of the Yanchang Formation in the Center of Ordos Basin

Research Institute of Exploration and Development of Changqing Oilfield Company,PetroChina,Xi'an710018;

Corresponding author: HE Jing

全文HTML

目录

友情链接

期刊在线

联系我们

通讯作者:
贺静