鄂尔多斯盆地高桥地区盒8段砂岩储层致密成因

陈大友; 朱玉双; 夏勇; 何磊; 何鎏; 艾庆琳; 薛云龙

doi:10.14027/j.cnki.cjxb.2015.06.014

ISSN 1000-0550 CN 62-1038/P

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鄂尔多斯盆地高桥地区盒8段砂岩储层致密成因

陈大友, 朱玉双, 夏勇, 何磊, 何鎏, 艾庆琳, 薛云龙

文章导航 > 沉积学报 > 2015 > 33(6): 1217-1223

陈大友, 朱玉双, 夏勇, 何磊, 何鎏, 艾庆琳, 薛云龙. 鄂尔多斯盆地高桥地区盒8段砂岩储层致密成因[J]. 沉积学报, 2015, 33(6): 1217-1223. doi: 10.14027/j.cnki.cjxb.2015.06.014

引用本文:

CHEN DaYou, ZHU YuShuang, XIA Yong, HE Lei, HE Liu, AI QingLin, XUE YunLong. Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1217-1223. doi: 10.14027/j.cnki.cjxb.2015.06.014

Citation:

CHEN DaYou, ZHU YuShuang, XIA Yong, HE Lei, HE Liu, AI QingLin, XUE YunLong. Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1217-1223. doi: 10.14027/j.cnki.cjxb.2015.06.014

引用本文:

Citation:

CHEN DaYou, ZHU YuShuang, XIA Yong, HE Lei, HE Liu, AI QingLin, XUE YunLong. Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1217-1223. doi: 10.14027/j.cnki.cjxb.2015.06.014

鄂尔多斯盆地高桥地区盒8段砂岩储层致密成因

doi: 10.14027/j.cnki.cjxb.2015.06.014

1.
西北大学地质学系大陆动力学国家重点实验室(西北大学) 西安 710069;
2.
中国石油长庆油田分公司勘探开发研究院西安 710018

基金项目: 国家科技重大专项(编号:2008ZX05013-005)与西北大学研究生自主创新项目(编号:YZZ13012)联合资助

详细信息

作者简介:
陈大友男 1987年出生博士研究生油气田地质与开发 E-mail:dychenhn@126.com

中图分类号: TE122.2

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文章访问数: 438
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PDF下载量: 718
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Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China

1.
Gedogy Department of Northwest University, State Key Laboratory of Continental Dynamics(Northwest University), Xi'an 710069;
2.
Research Instituie of Petroleum Exploration and Development, Changqing Oilfield Company, CNPC, Xi'an 710018

摘要

摘要: 运用常规薄片、铸体薄片、扫描电镜及恒速压汞等实验手段,对鄂尔多斯盆地高桥地区盒8段储层特征进行研究,并以孔隙演化过程为线索分析了储层致密成因。研究结果表明:盒8段储层主要为岩屑石英砂岩、石英砂岩与岩屑砂岩,成分成熟度和结构成熟度均较高,储层物性差;砂岩分选性好,初始孔隙度整体较高,平均可达34.7%;受岩石组分、埋深及煤系烃源岩酸性流体的影响,压实作用强烈,破坏了大约20.4%的原生孔隙度,胶结作用破坏了其余13.9%的原生孔隙度,原生孔隙几乎被破坏殆尽;早期溶蚀产生的孔隙被压实作用破坏,而晚期溶蚀作用较弱,仅增加了大约3.4%的次生孔隙度,难以大幅度改善储层物性。因此,成岩期原生孔隙被破坏殆尽及次生孔隙形成较少共同导致该区储层致密。
- 孔隙演化 /
- 致密成因 /
- 砂岩储层 /
- 盒8段 /
- 高桥地区 /
- 鄂尔多斯盆地
Abstract: Through conventional section, cast section, SEM samples and constant-rate mercury injection technology, characteristics of He 8 reservoir in Gaoqiao area of Ordos Basin were studied, and its origin mechanism of tightness was analysed based on pore evolution. The following conclusions were obtained. The rock types of He 8 reservoir were mainly lithic quartz sandstone, quartz sandstone and lithic sandstone, the compositional maturity and the textural maturity of sandstone were high, but its reservoir property was low. The selectivity of sandstone was good, the initial porosity overall was higher, about 34.7% on average. On the one hand, due to the effects of rock components, buried depth, acidic fluids of coal measure hydrocarbon source rock, and the compaction was strong, 20.4% primary porosity was destructed. On the other hand, cementation destroyed 13.9% of the remaining primary porosity, leading to the complete loss of most primary pore. The compaction was destructive for the pore formed by the early dissolution, at the same time, the later dissolution was weak, only increased by 3.4% secondary porosity, it was hard to improve the reservoir property remarkably. So, in the diagenesis stage, the complete loss of most primary pore and the less formation of secondary pore common lead to the tight reservoir.
- porosity evolution /
- origin mechanism of tightness /
- sandstone reservoirs /
- He 8 section /
- Gaoqiao area /
- Ordos Basin

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[1]	孙沛沛, 操应长, 远光辉, 周立宏, 靳子濠, 吴智平, 付立新, 张飞鹏, 陈长伟. 大港探区南部二叠系致密砂岩储层特征及成因 . 沉积学报, 2024, 42(4): 1447-1459. doi: 10.14027/j.issn.1000-0550.2023.090
[2]	曲希玉. 含体腔孔生物碎屑混积岩初始孔隙度恢复方法—以环渤中地区沙一二段混积岩储层为例 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.005
[3]	王炳森. 川中蓬莱地区震旦系灯影组四段储层成岩作用、孔隙演化及油气充注 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.012
[4]	徐宁宁, 张守鹏, 王永诗, 邱隆伟. 鄂尔多斯盆地北部二叠系下石盒子组致密砂岩成岩作用及孔隙成因 . 沉积学报, 2022, 40(2): 422-434. doi: 10.14027/j.issn.1000-0550.2021.027
[5]	马立元, 胡才志, 邱桂强, 陈纯芳, 高金慧, 徐士林. 鄂尔多斯盆地镇泾地区长8段储层非均质性及其结构模式 . 沉积学报, 2020, 38(5): 1088-1098. doi: 10.14027/j.issn.1000-0550.2020.039
[6]	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
[7]	潘星, 王海红, 王震亮, 刘一仓, 高徐辉, 王联国, 肖胜东. 三角洲平原砂岩差异成岩及其对储层分类的控制作用——以鄂尔多斯盆地西南部殷家城地区延安组为例 . 沉积学报, 2019, 37(5): 1031-1043. doi: 10.14027/j.issn.1000-0550.2018.182
[8]	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
[9]	陈贺贺, 朱筱敏, 陈纯芳, 尹伟, 施瑞生. 致密砂岩储层致密化与成藏史耦合关系研究——以鄂尔多斯南部镇原—泾川地区延长组长8油层组为例 . 沉积学报, 2018, 36(2): 401-414. doi: 10.14027/j.issn.1000-0550.2018.029
[10]	李树同, 时孜伟, 牟炜卫, 罗安湘, 王琪, 邓秀芹, 张文选, 李阳, 闫灿灿. 鄂尔多斯盆地西峰和姬塬油田长8₁段低渗透储层迥异性 . 沉积学报, 2018, 36(1): 166-175. doi: 10.3969/j.issn.1000-0550.2018.018
[11]	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
[12]	吴海枝, 韩润生, 邱文龙, 胡煜昭, 吴鹏. 楚雄盆地六苴铜矿床容矿砂岩孔隙演化对成矿的制约 . 沉积学报, 2015, 33(3): 512-523. doi: 10.14027/j.cnki.cjxb.2015.03.009
[13]	张辉, 王怀厂, 刘新社, 赵会涛. 古湖岸线确定及其对优质储集层控制——以鄂尔多斯盆地北部地区盒8段为例 . 沉积学报, 2015, 33(2): 348-356. doi: 10.14027/j.cnki.cjxb.2015.02.014
[14]	. 基于铸体薄片资料的砂岩储层孔隙度演化定量计算方法——以鄂尔多斯盆地环江地区长8储层为例 . 沉积学报, 2014, 32(2): 365-375.
[15]	杨华. 鄂尔多斯盆地周缘晚古生代火山活动对盆内砂岩储层的影响 . 沉积学报, 2007, 25(4): 526-534.
[16]	王琪, 禚喜准, 陈国俊, 史基安, 王多云. 鄂尔多斯盆地盐池—姬源地区三叠系长4+5砂岩成岩演化特征与优质储层分布 . 沉积学报, 2005, 23(3): 397-405.
[17]	李凤杰, 王多云, 宋广寿, 郑希民, 刘自亮, 王峰, 王志坤, 李树同. 陕甘宁盆地坳陷型湖盆缓坡带三角洲前缘短期基准面旋回与储层成因分析 . 沉积学报, 2004, 22(1): 73-78.
[18]	柳益群, 李文厚. 陕甘宁盆地东部上三叠统含油长石砂岩的成岩特点及孔隙演化 . 沉积学报, 1996, 14(3): 87-96.
[19]	薛莲花, 史基安, 晋慧娟. 辽河盆地沙河街组砂岩中碳酸盐胶结作用对孔隙演化控制机理研究 . 沉积学报, 1996, 14(2): 102-109.
[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.

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鄂尔多斯盆地高桥地区盒8段砂岩储层致密成因

doi: 10.14027/j.cnki.cjxb.2015.06.014

1. 西北大学地质学系大陆动力学国家重点实验室(西北大学) 西安 710069;

2. 中国石油长庆油田分公司勘探开发研究院西安 710018

基金项目: 国家科技重大专项(编号:2008ZX05013-005)与西北大学研究生自主创新项目(编号:YZZ13012)联合资助

作者简介:
陈大友男 1987年出生博士研究生油气田地质与开发 E-mail:dychenhn@126.com

收稿日期: 2015-04-03
修回日期: 2015-05-26
刊出日期: 2015-12-10

中图分类号: TE122.2

关键词:

盒8段 /

摘要: 运用常规薄片、铸体薄片、扫描电镜及恒速压汞等实验手段,对鄂尔多斯盆地高桥地区盒8段储层特征进行研究,并以孔隙演化过程为线索分析了储层致密成因。研究结果表明:盒8段储层主要为岩屑石英砂岩、石英砂岩与岩屑砂岩,成分成熟度和结构成熟度均较高,储层物性差;砂岩分选性好,初始孔隙度整体较高,平均可达34.7%;受岩石组分、埋深及煤系烃源岩酸性流体的影响,压实作用强烈,破坏了大约20.4%的原生孔隙度,胶结作用破坏了其余13.9%的原生孔隙度,原生孔隙几乎被破坏殆尽;早期溶蚀产生的孔隙被压实作用破坏,而晚期溶蚀作用较弱,仅增加了大约3.4%的次生孔隙度,难以大幅度改善储层物性。因此,成岩期原生孔隙被破坏殆尽及次生孔隙形成较少共同导致该区储层致密。

English Abstract

Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China

1. Gedogy Department of Northwest University, State Key Laboratory of Continental Dynamics(Northwest University), Xi'an 710069;

2. Research Instituie of Petroleum Exploration and Development, Changqing Oilfield Company, CNPC, Xi'an 710018

Received Date: 2015-04-03
Rev Recd Date: 2015-05-26
Publish Date: 2015-12-10

Keywords:

Abstract: Through conventional section, cast section, SEM samples and constant-rate mercury injection technology, characteristics of He 8 reservoir in Gaoqiao area of Ordos Basin were studied, and its origin mechanism of tightness was analysed based on pore evolution. The following conclusions were obtained. The rock types of He 8 reservoir were mainly lithic quartz sandstone, quartz sandstone and lithic sandstone, the compositional maturity and the textural maturity of sandstone were high, but its reservoir property was low. The selectivity of sandstone was good, the initial porosity overall was higher, about 34.7% on average. On the one hand, due to the effects of rock components, buried depth, acidic fluids of coal measure hydrocarbon source rock, and the compaction was strong, 20.4% primary porosity was destructed. On the other hand, cementation destroyed 13.9% of the remaining primary porosity, leading to the complete loss of most primary pore. The compaction was destructive for the pore formed by the early dissolution, at the same time, the later dissolution was weak, only increased by 3.4% secondary porosity, it was hard to improve the reservoir property remarkably. So, in the diagenesis stage, the complete loss of most primary pore and the less formation of secondary pore common lead to the tight reservoir.

引用本文:

Citation:

CHEN DaYou, ZHU YuShuang, XIA Yong, HE Lei, HE Liu, AI QingLin, XUE YunLong. Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China[J]. Acta Sedimentologica Sinica, 2015, 33(6): 1217-1223. doi: 10.14027/j.cnki.cjxb.2015.06.014

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鄂尔多斯盆地高桥地区盒8段砂岩储层致密成因

doi: 10.14027/j.cnki.cjxb.2015.06.014

作者简介:
陈大友男 1987年出生博士研究生油气田地质与开发 E-mail:dychenhn@126.com

计量

Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China

计量

目录

鄂尔多斯盆地高桥地区盒8段砂岩储层致密成因

doi: 10.14027/j.cnki.cjxb.2015.06.014

1. 西北大学地质学系大陆动力学国家重点实验室(西北大学) 西安 710069;

2. 中国石油长庆油田分公司勘探开发研究院西安 710018

作者简介:
陈大友男 1987年出生博士研究生油气田地质与开发 E-mail:dychenhn@126.com

English Abstract

Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China

1. Gedogy Department of Northwest University, State Key Laboratory of Continental Dynamics(Northwest University), Xi'an 710069;

2. Research Instituie of Petroleum Exploration and Development, Changqing Oilfield Company, CNPC, Xi'an 710018

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鄂尔多斯盆地高桥地区盒8段砂岩储层致密成因

doi: 10.14027/j.cnki.cjxb.2015.06.014

作者简介: 陈大友 男 1987年出生 博士研究生 油气田地质与开发 E-mail:dychenhn@126.com

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Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China

计量

出版历程

目录

鄂尔多斯盆地高桥地区盒8段砂岩储层致密成因

doi: 10.14027/j.cnki.cjxb.2015.06.014

1. 西北大学地质学系大陆动力学国家重点实验室(西北大学) 西安 710069; 2. 中国石油长庆油田分公司勘探开发研究院 西安 710018

作者简介: 陈大友 男 1987年出生 博士研究生 油气田地质与开发 E-mail:dychenhn@126.com

English Abstract

Origin Mechanism of Tightness from the He 8 Section Sandstone Reservoir in Gaoqiao Area of Ordos Basin, China

1. Gedogy Department of Northwest University, State Key Laboratory of Continental Dynamics(Northwest University), Xi'an 710069; 2. Research Instituie of Petroleum Exploration and Development, Changqing Oilfield Company, CNPC, Xi'an 710018

全文HTML

目录

友情链接

期刊在线

联系我们

作者简介:
陈大友男 1987年出生博士研究生油气田地质与开发 E-mail:dychenhn@126.com

1. 西北大学地质学系大陆动力学国家重点实验室(西北大学) 西安 710069;

2. 中国石油长庆油田分公司勘探开发研究院西安 710018

作者简介:
陈大友男 1987年出生博士研究生油气田地质与开发 E-mail:dychenhn@126.com

1. Gedogy Department of Northwest University, State Key Laboratory of Continental Dynamics(Northwest University), Xi'an 710069;

2. Research Instituie of Petroleum Exploration and Development, Changqing Oilfield Company, CNPC, Xi'an 710018