苏里格气田西区盒8下亚段辫状河沉积论证与分析

doi:10.13278/j.cnki.jjuese.201506104

吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (6): 1597-1607.doi: 10.13278/j.cnki.jjuese.201506104

苏里格气田西区盒₈^下亚段辫状河沉积论证与分析

单敬福¹, 张吉^2,3, 王继平^2,3, 赵忠军^2,3, 李浮萍^2,3, 陈治华^2,3, 石林辉^2,3, 刘利峰^2,3

1. 长江大学油气资源与勘探技术教育部重点实验室, 武汉 430100;
2. 中国石油长庆油田分公司苏里格气田研究中心, 西安 710018;
3. 低渗透油气田勘探开发国家工程实验室, 西安 710018

收稿日期:2014-12-02 发布日期:2015-11-26
作者简介:单敬福(1977),男,副教授,博士,主要从事沉积、储层与开发地质学研究工作,E-mail:shanjingfu2003@163.com。
基金资助:
国家自然科学基金项目(41372125);湖北省教育厅基金项目(Q20121210);中国地质大学(武汉)构造与油气资源教育部重点实验室开放基金(TPR-2012-23)

Demenstration and Analysis of Braided River Deposition in the Lower He₈ Member in Western Sulige Gas Field

Shan Jingfu¹, Zhang Ji^2,3, Wang Jiping^2,3, Zhao Zhongjun^2,3, Li Fuping^2,3, Chen Zhihua^2,3, Shi Linhui^2,3, Liu Lifeng^2,3

1. Key Laboratory of Exploration Technologies for Oil and Gas Resources, MOE, Yangtze University, Wuhan 430100, China;
2. Research Center of Sulige Gas Field, Changqing Oilfield Company, PetroChina, Xi'an 710018, China;
3. National Engineering Laboratory for Exploration and Development of Low-Permeability Oil & Gas Fields, Xi'an 710018, China

Received:2014-12-02 Published:2015-11-26

摘要/Abstract

摘要：

鄂尔多斯盆地苏里格气田西区盒₈^下亚段主力含气层段相的研究观点较多,不同认识导致各个沉积相域内砂体对比和预测存在着较大的差异,从而给勘探井位部署增加了难度。笔者在前人研究成果基础上,充分利用钻井、测井、岩心、地震、分析化验和野外露头等多种资料和手段,采用岩石学特征分析、岩心沉积构特征观察、古生物化石证据、研究区柳林成家庄野外露头沉积序列揭示、测井相特征和河流相地震特殊反射结构观察等多种研究手段和方法,对该区盒₈^下亚段的沉积相进行了详细论证、分析和描述。研究结果表明,辫状河沉积是苏里格西区盒₈^下亚段主要的相类型;干旱与潮湿气候的频繁交替变化,是导致砂体研究区目的层垂向砂体厚度大、非均质性强和砂体横向变化快的主控因素。

关键词: 苏里格气田西区, 辫状河, 盒₈^下亚段, 沉积模式

Abstract:

The opinions to the sedimentary facies in the western Sulige gas field were so different that they lead to the big difficulty to forecast the sandbody distribution in exploration and development. We studied the sedimentary facies through adopting the techniques and methods of stone characteristics analysis, sedimentary structure description, and fossil observation; revealed sedimentary sequences of outcrop from Chengjiazhuang based on the facies logging and seismic reflection related to fluvial facies researched by predecessors in the Lower He₈ Member. The research results show that the braided river deposition is the main facies type of the Lower He₈ Member in Western Sulige Gas Field. In our opinion, the frequent climate change from dry to humid is the controlling factor,which resulted in the large thickness of sandbody, strong heterogeneity, and lateral variation of reservoir.

Key words: western Sulige gas field, braided river, Lower He 8 Member, sedimentary model

中图分类号:

P618.13

单敬福, 张吉, 王继平, 赵忠军, 李浮萍, 陈治华, 石林辉, 刘利峰. 苏里格气田西区盒₈^下亚段辫状河沉积论证与分析[J]. 吉林大学学报(地球科学版), 2015, 45(6): 1597-1607.

Shan Jingfu, Zhang Ji, Wang Jiping, Zhao Zhongjun, Li Fuping, Chen Zhihua, Shi Linhui, Liu Lifeng. Demenstration and Analysis of Braided River Deposition in the Lower He₈ Member in Western Sulige Gas Field[J]. Journal of Jilin University(Earth Science Edition), 2015, 45(6): 1597-1607.

参考文献

[1] 何顺利, 兰朝利, 门成全. 苏里格气田储层的新型辫状河沉积模式[J].石油学报,2005,26(6):25-29. He Shunli, Lan Chaoli, Men Chengquan. New Braided River Model in Sulige Gas Field of Ordos Basin[J]. Acta Petrolei Sinica, 2005,26(6):25-29.

[2] 朱红涛, 陈开远, Liu Keyu,等. 鄂尔多斯盆地东北部山西组河流相沉积证据[J].天然气工业,2007,27(12):68-70. Zhu Hongtao, Chen Kaiyuan, Liu Keyu, et al. Evidences for Deposits of Fluvial Facies in Shanxi Formation in Northeastern Ordos Basin[J]. Natural Gas Industry, 2007,27(12):68-70.

[3] 陈孟晋,汪泽成,郭彦如,等.鄂尔多斯盆地南部晚古生代沉积特征与天然气勘探潜力[J].石油勘探与开发, 2006,33(1):1-5. Chen Mengjin, Wang Zecheng, Guo Yanru, et al. Late Paleozoic Sedimentary Systems and Gas Potential in the South Ordos Basin[J]. Petroleum Exploration and Development, 2006,33(1):1-5.

[4] 杨西燕,沈昭国,方少仙,等.鄂尔多斯盆地乌审旗气田中二叠统下石盒子组盒₈段下亚段滩坝砂体沉积特征[J].古地理学报,2007,9(2):175-183. Yang Xiyan, Shen Zhaoguo, Fang Shaoxian, et al. Sedimentary Characteristics of Beach and Bar Sandbodies in the Lower Submember of Member 8 of Xiashihezi Formation of Middle Permian in Wushenqi Gas Field, Ordos Basin[J]. Journal of Palaeogeography, 2007,9(2):175-183.

[5] 徐蒙,王家豪,徐东浩,等.苏里格气田苏120区块盒₈段浅水辫状河三角洲砂体演化规律[J].沉积学报,2013,31(2):340-349. Xu Meng, Wang Jiahao, Xu Donghao, et al. The Sandbody Evolution of Shallow-Water Braided River Deltas in the Earth Member of Shihezi Formation in Block Su120, Sulige Gas Field[J]. Acta Sedimentologica Sinica, 2013,31(2):340-349.

[6] 刘建新,雍学善,吴会良,等. 苏里格气田盒8段地震多技术储层沉积相研究[J].岩性油气藏,2007, 19(2):80-83. Liu Jianxin, Yong Xueshan, Wu Huiliang, et al. Study on Sedimentary Facies by Seismic Multiple Techniques in the Eighth Member of Shihezi Formation, Sulig Gas Field[J]. Lithologic Reservoir, 2007, 19(2):80-83.

[7] 刘行军,张吉,尤世梅. 苏里格中部地区盒8段储层沉积相控测井解释分析[J].测井技术,2008,32(3):228-232. Liu Xingjun, Zhang Ji, You Shimei. Logging Interpretation of Sedimentary Facies Controlled Reservoir in Central Sulige[J].Well Logging Technology, 2008,32(3):228-232.

[8] 文华国,郑荣才,高红灿,等. 苏里格气田苏6井区下石盒子组盒₈段沉积相特征[J]. 沉积学报,2007, 25(1):90-98. Wen Huaguo, Zheng Rongcai, Gao Hongcan, et al. Sedimentary Facies of the 8th Member of Lower Shihezi Formation in Su6 Area, Sulige Gas Field[J]. Acta Sedimentologica Sinica, 2007,25(1):90-98.

[9] Visher G S. Grain Size Distributions and Depositional Processes[J]. Jour Sed Petro, 1969, 39:1074-1106.

[10] Miall A D.Reservoir Heterogeneities in Fluvial Sand-stones:Lessons from Outcrop Studies[J]. AAPG Bulletin,1988,72:682-697.

[11] Robert L Folk, Siedlecka Anna. The "Schizohaline" Environment: Its Sedimentary and Diagenetic Fabrics as Exemplified by Late Paleozoic Rocks of Bear Island, Svalbard[J]. Sedimentary Geology, 1974, 11(1):1-15.

[12] 白振华,詹燕涛,王赢,等. 苏里格气田苏14井区盒8段河流相砂体展布与演化规律研究[J]. 岩性油气藏,2013,25(1):56-62. Bai Zhenhua, Zhan Yantao, Wang Lei, et al. Fluvial Sand Bodies Distribution and Evolution of He8 Member in Su14 Block of Sulige Gas Field[J]. Lithologic Reservoir, 2013,25(1):56-62.

[13] 费世祥,冯强汉,安志伟,等. 苏里格气田中区下石盒子组盒8段沉积相研究[J].天然气勘探与开发,2013,36(2):17-22,85. Fei Shixiang, Feng Qianghan, An Zhiwei, et al. Sedimentary Facies of Shihezi 8 Member in Middle Area, Sulige Gas Field[J]. Natural Gas Exploration & Development, 2013, 36(2):17-22,85.

[14] 叶亮,叶武,蔡泉,等. 苏里格气田S158井区盒8段沉积相平面展布特征[J].天然气技术与经济,2013, 7(2):10-14,28,77. Ye Liang, Ye Wu, Cai Quan, et al. Planar Distribution of Sedimentary Facies in Shihezi 8 Member of S158 Well Block,Sulige Gas Field[J]. Natural Gas Technology and Economy, 2013,7(2):10-14,28,77.

[15] 李顺明,宋新民,刘曰强,等.温米退积型与进积型浅水辫状河三角洲沉积模式[J].吉林大学学报:地球科学版,2011,41(3):665-672. Li Shunming, Song Xinmin, Liu Yueqiang, et al. Depositional Models of Regressive and Progressive Shoal Braided Deltas in Wenmi Oilfield[J]. Journal of Jilin University:Earth Science Edition, 2011,41(3):665-672.

Metrics

Viewed

Full text

441

HTML			PDF

Just accepted	Online first	Issue	Just accepted	Online first	Issue
0	0	0	0	0	441

From	Others	local

Times	137	304
Rate	31%	69%

Abstract

414

Just accepted	Online first	Issue

0	0	414

From	Others	local

Times	390	24
Rate	94%	6%

Cited

Web of Science	Crossref	ScienceDirect	Search for Citations in Google Scholar >>


This page requires you have already subscribed to WoS.

Shared

Discussed

苏里格气田西区盒₈^下亚段辫状河沉积论证与分析

Demenstration and Analysis of Braided River Deposition in the Lower He₈ Member in Western Sulige Gas Field

PDF (PC)

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 10

Metrics

本文评价

推荐阅读 0

[1]	朱兆群, 林承焰, 张宪国, 李志鹏, 谢晶晶, 魏肃东, 程平. 断陷湖盆早期浅水三角洲沉积——以高邮凹陷永安地区戴一段为例[J]. 吉林大学学报(地球科学版), 2017, 47(3): 659-673.
[2]	张建坤, 杨国涛, 吴吉忠, 吴鑫, 王方鲁. 黄骅坳陷北部马头营凸起馆陶组砂体成因及展布特征[J]. 吉林大学学报(地球科学版), 2017, 47(1): 48-60.
[3]	张晶, 刘化清, 李双文, 冀虎山, 袁淑琴, 洪忠. 断陷湖盆深水重力流水道的识别标志及沉积模式——以歧口凹陷歧南斜坡沙一段为例[J]. 吉林大学学报(地球科学版), 2015, 45(3): 701-711.
[4]	李顺明, 宋新民, 刘曰强, 王友启, 李艳明, 唐后军. 温米退积型与进积型浅水辫状河三角洲沉积模式[J]. J4, 2011, 41(3): 665-672.
[5]	伊振林, 吴胜和, 杜庆龙, 张保国, 岳大力, 李艳平. 冲积扇储层构型精细解剖方法--以克拉玛依油田六中区下克拉玛依组为例[J]. J4, 2010, 40(4): 939-946.
[6]	孔庆莹, 程日辉. 塔里木盆地孔雀河地区寒武系-下奥陶统沉积特征[J]. J4, 2010, 40(3): 527-534.
[7]	王蛟. 山东沾化凹陷孤岛油田馆上段浅水湖泊沉积[J]. J4, 2007, 37(3): 500-0505.
[8]	张晶,王伟锋,荣启宏,史文东. 东营凹陷永55区块沙四上亚段深水浊积扇沉积与油气[J]. J4, 2007, 37(3): 519-0524.
[9]	张健,刘招君,杜江峰,柳蓉,王伟涛,柳世友,荆保泽. 黑龙江省依兰盆地古近系达连河组油页岩沉积特征[J]. J4, 2006, 36(6): 980-0985.
[10]	王蛟，姜在兴，操应长，邢焕清，王艳忠，罗文生. 山东东营凹陷永921地区沙四上亚段扇三角洲沉积与油气[J]. J4, 2005, 35(06): 725-0731.