伊朗西南部上白垩统Sarvak组储层特征及主控因素

杜洋; 郑淑芬; 龚勋; 陈秋实; 汪娟; 辛军; 陈杰

doi:10.14027/j.cnki.cjxb.2016.01.013

ISSN 1000-0550 CN 62-1038/P

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伊朗西南部上白垩统Sarvak组储层特征及主控因素

杜洋, 郑淑芬, 龚勋, 陈秋实, 汪娟, 辛军, 陈杰

文章导航 > 沉积学报 > 2016 > 34(1): 137-148

杜洋, 郑淑芬, 龚勋, 陈秋实, 汪娟, 辛军, 陈杰. 伊朗西南部上白垩统Sarvak组储层特征及主控因素[J]. 沉积学报, 2016, 34(1): 137-148. doi: 10.14027/j.cnki.cjxb.2016.01.013

引用本文:

DU Yang, ZHENG ShuFen, GONG Xun, CHEN QiuShi, WANG Juan, XIN Jun, CHEN Jie. Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran[J]. Acta Sedimentologica Sinica, 2016, 34(1): 137-148. doi: 10.14027/j.cnki.cjxb.2016.01.013

Citation:

DU Yang, ZHENG ShuFen, GONG Xun, CHEN QiuShi, WANG Juan, XIN Jun, CHEN Jie. Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran[J]. Acta Sedimentologica Sinica, 2016, 34(1): 137-148. doi: 10.14027/j.cnki.cjxb.2016.01.013

引用本文:

Citation:

DU Yang, ZHENG ShuFen, GONG Xun, CHEN QiuShi, WANG Juan, XIN Jun, CHEN Jie. Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran[J]. Acta Sedimentologica Sinica, 2016, 34(1): 137-148. doi: 10.14027/j.cnki.cjxb.2016.01.013

伊朗西南部上白垩统Sarvak组储层特征及主控因素

doi: 10.14027/j.cnki.cjxb.2016.01.013

杜洋^1,2,
郑淑芬²,
龚勋²,
陈秋实²,
汪娟²,
辛军²,
陈杰²

1.
西南石油大学地球科学与技术学院成都 610000;
2.
川庆钻探工程公司地质勘探开发研究院成都 610051

基金项目: 中国石油天然气集团公司重大科技专项(11.2011E-2501.X.01)

详细信息

中图分类号: P618.13

计量

文章访问数: 493
HTML全文浏览量: 5
PDF下载量: 872
被引次数: 0

Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran

1.
Southwest Petroleum Universtiy, Chengdu 610000, China;
2.
Geology and Exploration Research Institute of CCDC, CNPC, Chengdu 610051, China

Funds: Key Science and Technology Programs of China National Petroleum Company, No.11.2011E-2501.X.01

摘要

摘要: 运用取芯,薄片,电镜扫描及三维地震等资料,对位于扎格罗斯盆地盆缘当前热点开发区的伊朗A油田上白垩统Sarvak组储层特征及主控因素进行研究。研究表明:Sarvak组储层岩性以富含厚壳蛤、有孔虫、钙化藻和浮游有孔虫等生屑颗粒的灰岩和白垩灰岩为主。储层受岩溶作用影响明显,储集空间以生屑铸模孔,灰泥溶蚀孔群,溶孔,溶洞为主。结合压汞,孔渗关系,岩性等因素在层内综合划分出孔洞—孔隙型,裂缝—孔隙型,孔隙型和致密非储层四类。最有利储层为孔洞—孔隙型,岩性主要为富厚壳蛤碎屑灰岩,次有利储层为裂缝—孔隙型和孔隙型,岩性主要为富有孔虫碎屑白垩灰岩。储层主控因素为层内三级层序边界,古地貌隆起和岩石破裂作用。三级层序边界控制有利储层垂向位置,古地貌隆起控制储层性质平面分布,岩石破裂作用影响储层整体含油性。基于以上认识提出勘探开发建议:对层内三级界面的识别和明确原沉积期古隆起位置为确定油田垂向优先开发层位及平面有利开发区域的关键。距层序界面较远,厚度较大的白垩储层受岩石破裂作用影响较大,纵横向分布发育不稳定,储量计算应考虑对纵向不同类别储层进行分类评价。
- 伊朗 /
- 扎格罗斯盆地 /
- Sarvak /
- 岩溶作用 /
- 储层主控因素 /
- 勘探开发建议
Abstract: This paper studys on the characteristics and main controlling factors of the upper Cretaceous Sarvak reservoir by the coring, section, SEM, well logging and 3D seismic data. The study area is the Azadegan oilfield of the SouthWest, Iran and which situated in the "hot zone" of the Zagros foreland basin nowadays. The main lithology of the Sarvak is the limestone and chalk limestone which is abundant of the rudist, foraminifer debris. The reservoir is influenced by the multi-stage of the karstification effect and the effect reservoir space is the moldic pore, cavern, vug, and mud matrix dissolved pore. According to the MISC, por-per relationship and lithology, we divided the reservoir into four types that are vug-pore, fracture-pore, matrix pore and non-reservoir. The optimum is the vug-pore and the mainly is the rudist bearing reservoir, and the secondary reservoir is the fracture-pore and the matrix pore reservoir, and mainly is the foraminifer bearing chalk limestone. The reservoir main controlling factor are the 3rd Squence boundary, palaeogeomorphology of the depositional time and rock fracturing by the multi-stage tectonic activities. The Squence boundary control the vertical position of optimum reservoir, the palaeogeomorphology control the lateral reservoir quality distribution, and the rock fracturing control the oiliness property of the chalky limestone. According to these findings, we propose the development suggestions as below: Clearing the 3^rd sequence boundary of inner formation and the paleo-high of depositional time is the critical factors to select the favorable vertical develop zone and lateral develop area. The reservoir quality and oiliness of the thick chalk limestone is influenced by the rock fracturing, and is more unstable compare with the reservoir zone near the sequence boundary. So, at the early stage of the field development, we should consider the grading evaluation criteria in the reserves calculation.
- Iran /
- Zagros Basin /
- Sarvak /
- Karsitfication /
- reservoir controlling factor /
- development suggestion

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[1]	刘邦, 张新新, 翟光华, 袁圣强, 王中凡, 王崇. 尼日尔Termit盆地Trakes斜坡上白垩统Donga组海相砂岩储层特征及主控因素 . 沉积学报, 2024, (): -. doi: 10.14027/j.issn.1000-0550.2024.027
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[8]	张金友. 陆相坳陷盆地烃源岩内致密砂岩储层含油性主控因素——以松辽盆地北部中央坳陷区齐家凹陷高台子油层为例 . 沉积学报, 2016, 34(5): 991-1002. doi: 10.14027/j.cnki.cjxb.2016.05.018
[9]	杜洋, 辛军, 徐乾承, 陈杰, 李宜真, 汪娟, 童明胜. 基于储层结构的厚壳蛤建隆沉积模式——以伊朗SA油田Sarvak油藏为例 . 沉积学报, 2015, 33(6): 1247-1257. doi: 10.14027/j.cnki.cjxb.2015.06.017
[10]	斯春松, 刘占国, 寿建峰, 李积永, 宫清顺, 张庆丰, 王鹏, 王波. 柴达木盆地昆北地区路乐河组砂砾岩有效储层发育主控因素及分布规律 . 沉积学报, 2014, 32(5): 966-972.
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[14]	陈景山. 塔里木盆地奥陶系碳酸盐岩古岩溶作用与储层分布 . 沉积学报, 2007, 25(6): 858-868.
[15]	马达德, 寿建峰, 胡勇, 王少依, 徐宁. 柴达木盆地柴西南区碎屑岩储层形成的主控因素分析 . 沉积学报, 2005, 23(4): 589-595.
[16]	刘忠宝, 于炳松, 李廷艳, 樊太亮, 蒋宏忱. 塔里木盆地塔中地区中上奥陶统碳酸盐岩层序发育对同生期岩溶作用的控制 . 沉积学报, 2004, 22(1): 103-109.
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[18]	金振奎, 邹元荣, 蒋春雷, 由伟丰. 大港探区奥陶系岩溶储层发育分布控制因素 . 沉积学报, 2001, 19(4): 530-535.
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伊朗西南部上白垩统Sarvak组储层特征及主控因素

doi: 10.14027/j.cnki.cjxb.2016.01.013

1. 西南石油大学地球科学与技术学院成都 610000;

2. 川庆钻探工程公司地质勘探开发研究院成都 610051

基金项目: 中国石油天然气集团公司重大科技专项(11.2011E-2501.X.01)

收稿日期: 2015-04-07
修回日期: 2015-05-20
刊出日期: 2016-02-10

中图分类号: P618.13

关键词:

伊朗 /

Sarvak /

摘要: 运用取芯,薄片,电镜扫描及三维地震等资料,对位于扎格罗斯盆地盆缘当前热点开发区的伊朗A油田上白垩统Sarvak组储层特征及主控因素进行研究。研究表明:Sarvak组储层岩性以富含厚壳蛤、有孔虫、钙化藻和浮游有孔虫等生屑颗粒的灰岩和白垩灰岩为主。储层受岩溶作用影响明显,储集空间以生屑铸模孔,灰泥溶蚀孔群,溶孔,溶洞为主。结合压汞,孔渗关系,岩性等因素在层内综合划分出孔洞—孔隙型,裂缝—孔隙型,孔隙型和致密非储层四类。最有利储层为孔洞—孔隙型,岩性主要为富厚壳蛤碎屑灰岩,次有利储层为裂缝—孔隙型和孔隙型,岩性主要为富有孔虫碎屑白垩灰岩。储层主控因素为层内三级层序边界,古地貌隆起和岩石破裂作用。三级层序边界控制有利储层垂向位置,古地貌隆起控制储层性质平面分布,岩石破裂作用影响储层整体含油性。基于以上认识提出勘探开发建议:对层内三级界面的识别和明确原沉积期古隆起位置为确定油田垂向优先开发层位及平面有利开发区域的关键。距层序界面较远,厚度较大的白垩储层受岩石破裂作用影响较大,纵横向分布发育不稳定,储量计算应考虑对纵向不同类别储层进行分类评价。

English Abstract

Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran

1. Southwest Petroleum Universtiy, Chengdu 610000, China;

2. Geology and Exploration Research Institute of CCDC, CNPC, Chengdu 610051, China

Funds: Key Science and Technology Programs of China National Petroleum Company, No.11.2011E-2501.X.01

Received Date: 2015-04-07
Rev Recd Date: 2015-05-20
Publish Date: 2016-02-10

Keywords:

Abstract: This paper studys on the characteristics and main controlling factors of the upper Cretaceous Sarvak reservoir by the coring, section, SEM, well logging and 3D seismic data. The study area is the Azadegan oilfield of the SouthWest, Iran and which situated in the "hot zone" of the Zagros foreland basin nowadays. The main lithology of the Sarvak is the limestone and chalk limestone which is abundant of the rudist, foraminifer debris. The reservoir is influenced by the multi-stage of the karstification effect and the effect reservoir space is the moldic pore, cavern, vug, and mud matrix dissolved pore. According to the MISC, por-per relationship and lithology, we divided the reservoir into four types that are vug-pore, fracture-pore, matrix pore and non-reservoir. The optimum is the vug-pore and the mainly is the rudist bearing reservoir, and the secondary reservoir is the fracture-pore and the matrix pore reservoir, and mainly is the foraminifer bearing chalk limestone. The reservoir main controlling factor are the 3rd Squence boundary, palaeogeomorphology of the depositional time and rock fracturing by the multi-stage tectonic activities. The Squence boundary control the vertical position of optimum reservoir, the palaeogeomorphology control the lateral reservoir quality distribution, and the rock fracturing control the oiliness property of the chalky limestone. According to these findings, we propose the development suggestions as below: Clearing the 3^rd sequence boundary of inner formation and the paleo-high of depositional time is the critical factors to select the favorable vertical develop zone and lateral develop area. The reservoir quality and oiliness of the thick chalk limestone is influenced by the rock fracturing, and is more unstable compare with the reservoir zone near the sequence boundary. So, at the early stage of the field development, we should consider the grading evaluation criteria in the reserves calculation.

引用本文:

Citation:

DU Yang, ZHENG ShuFen, GONG Xun, CHEN QiuShi, WANG Juan, XIN Jun, CHEN Jie. Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran[J]. Acta Sedimentologica Sinica, 2016, 34(1): 137-148. doi: 10.14027/j.cnki.cjxb.2016.01.013

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伊朗西南部上白垩统Sarvak组储层特征及主控因素

doi: 10.14027/j.cnki.cjxb.2016.01.013

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Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran

计量

目录

伊朗西南部上白垩统Sarvak组储层特征及主控因素

doi: 10.14027/j.cnki.cjxb.2016.01.013

1. 西南石油大学地球科学与技术学院成都 610000;

2. 川庆钻探工程公司地质勘探开发研究院成都 610051

English Abstract

Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran

1. Southwest Petroleum Universtiy, Chengdu 610000, China;

2. Geology and Exploration Research Institute of CCDC, CNPC, Chengdu 610051, China

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伊朗西南部上白垩统Sarvak组储层特征及主控因素

doi: 10.14027/j.cnki.cjxb.2016.01.013

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出版历程

Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran

计量

出版历程

目录

伊朗西南部上白垩统Sarvak组储层特征及主控因素

doi: 10.14027/j.cnki.cjxb.2016.01.013

1. 西南石油大学地球科学与技术学院 成都 610000; 2. 川庆钻探工程公司地质勘探开发研究院 成都 610051

English Abstract

Characteristics and Main Controlling Factor of the Upper Cretaceous Sarvak Reservoir, SouthWest Iran

1. Southwest Petroleum Universtiy, Chengdu 610000, China; 2. Geology and Exploration Research Institute of CCDC, CNPC, Chengdu 610051, China

全文HTML

目录

友情链接

期刊在线

联系我们

1. 西南石油大学地球科学与技术学院成都 610000;

2. 川庆钻探工程公司地质勘探开发研究院成都 610051

1. Southwest Petroleum Universtiy, Chengdu 610000, China;

2. Geology and Exploration Research Institute of CCDC, CNPC, Chengdu 610051, China