土库曼斯坦阿姆河右岸地区盐下碳酸盐岩气藏类型及油气富集因素

聂明龙; 童晓光; 刘群明; 徐树宝; 吴蕾; 陈骁帅; 禚喜准

doi:10.11781/sysydz201601070

土库曼斯坦阿姆河右岸地区盐下碳酸盐岩气藏类型及油气富集因素

doi: 10.11781/sysydz201601070

1.
辽宁工程技术大学, 辽宁葫芦岛 125105
2. 中国地质大学(北京)能源学院, 北京 100083
3. 中国石油天然气勘探开发公司, 北京 100034
4. 中国石油勘探开发研究院, 北京 100083
5. 中国石油(土库曼斯坦)阿姆河天然气公司, 土库曼斯坦阿什哈巴德

基金项目: 国家青年基金(41402101)和国家科技重大专项(2011ZX-05059)联合资助。

详细信息

作者简介:
聂明龙(1976-),男,博士后,从事油气地质综合研究及教学工作。E-mail:nieminglong@sohu.com。

中图分类号: TE122.3
计量
- 文章访问数: 1421
- HTML全文浏览量: 135
- PDF下载量: 1076
- 被引次数: 0
出版历程
- 收稿日期: 2015-01-23
- 修回日期: 2015-12-11
- 刊出日期: 2016-01-28

Types of pre-salt carbonate gas reservoirs and hydrocarbon enrichment factors of Amu Darya right bank area in Turkmenistan

1.
Liaoning Technical University, Huludao, Liaoning 125105, China
2. School of Energy Resources, China University of Geosciences(Beijing), Beijing 100083, China
3. China National Oil and Gas Exploration and Development Corporation, Beijing 100034, China
4. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China
5. CNPC(Turkmenistan) Amu Darya River Gas Company, Ashkhabad, Turkmenistan

摘要

摘要: 土库曼斯坦阿姆河右岸地区盐下中上侏罗统卡洛夫-牛津阶碳酸盐岩油气资源丰富,但是油气分布规律的研究相对滞后,通过对典型气藏解剖,分析了油气藏类型,探讨了油气富集高产的主控因素。结果表明,该区盐下碳酸盐岩发育有构造气藏、岩性气藏和构造-岩性复合气藏3大类及背斜气藏、断背斜气藏、逆冲断裂背斜气藏、生物礁岩性气藏和构造-岩性气藏等5小类气藏。海西期基底古隆起控制了大气田的形成,喜马拉雅期挤压构造运动形成了逆冲断裂油气聚集带,沉积相带控制了气藏含油气丰度,盐膏岩盖层保存条件好,形成断背斜气藏。大型完整背斜构造与高能礁滩体相配,是西部查尔朱阶地天然气富集高产的主控因素;逆冲断裂背斜构造圈闭与大规模的缝洞型储集体配合,是东部别什肯特坳陷和基萨尔褶皱隆起区天然气富集高产的主控因素。
- 盐膏岩 /
- 礁滩体 /
- 气藏类型 /
- 富集因素 /
- 阿姆河盆地 /
- 土库曼斯坦
Abstract: Hydrocarbon resources in the Middle-Upper Jurassic Callovian-Oxfordian carbonate rocks are abundant; however, research on the distribution law of hydrocarbon is relatively backward. Through the study of typical gas reservoirs, analysis of the type of hydrocarbon reservoirs and discussion of the major reasons for high hydrocarbon output, we determined that there are three main types of pre-salt gas reservoirs in carbonate rocks:structural, lithologic and structural-lithologic compound gas reservoirs. Additionally, there are five minor gas reservoirs:anticline, faulted anticline, thrust faulted anticline, reefs and structural-lithologic gas reservoirs. We also discovered that Hercynian basement paleo-uplift controlled the formation of large gas fields and Himalayan extruded tectonic movement formed thrust faulted hydrocarbon accumulation zones. The abundance of gas was controlled by sedimentary facies belts and good seal provided by salt-gypsum cover contributing to the formation of faulted anticline gas reservoirs. The coincidence of large anticline structures and high energy reef beach body was the major controlling factor for the enrichment of natural gas in the west Zarzhu terrace. The coincidence of thrust faulted anticlinal structural traps and large scale fissure type reservoirs is the main reason for the enrichment and high yield of natural gas in the east Bieshikent Depression and Jisaer folded uplift zone.
- salt-gypsum rock /
- reef beach body /
- types of gas reservoirs /
- enrichment factors /
- Amu Darya Basin /
- Turkmenistan

HTML全文

参考文献(18)

[1]	Warren J K.Evaporites:sediments,resources and hydrocarbons[M].Berlin:Springer,2006:1052.
[2]	郭永强,刘洛夫,朱胜利,等.阿姆达林盆地含油气系统划分与评价[J].石油勘探与开发,2006,33(4):515-520. Guo Yongqiang,Liu Luofu,Zhu Shengli,et al.Classification and assessment of petroleum system in Amu-Daria Basin[J].Petroleum Exploration and Development,2006,33(4):515-520.
[3]	李浩武,童晓光,王素花,等.阿姆河盆地侏罗系成藏组合地质特征及勘探潜力[J].天然气工业,2010,30(5):6-12. Li Haowu,Tong Xiaoguang,Wang Suhua,et al.An analysis of geological characteristics and exploration potential of the Jurassic play,Amu Darya Basin[J].Natural Gas Industry,2010,30(5):6-12.
[4]	费怀义,徐刚,王强,等.阿姆河右岸区块气藏特征[J].天然气工业,2010,30(5):13-17. Fei Huaiyi,Xu Gang,Wang Qiang,et al.Characteristics of gas reservoirs in the Amu Darya Right Bank Block,Turkmenistan[J].Natural Gas Industry,2010,30(5):13-17.
[5]	徐剑良,程绪彬,吴蕾,等.阿姆河右岸区块构造演化与成藏条件[J].天然气工业,2010,30(5):18-20. Xu Jianliang,Cheng Xubin,Wu Lei,et al.Structural evolution and hydrocarbon pooling conditions in the Amu Darya Right Bank Block,Turkmenistan[J].Natural Gas Industry,2010,30(5):18-20.
[6]	刘洛夫,朱毅秀.滨里海盆地及中亚地区油气地质特征[M].北京:中国石化出版社,2007:18-38. Liu Luofu,Zhu Yixiu.Characteristics of petroleum geology in Caspian Basin and central Asiaarea[M].Beijing:China Petrochemical Press,2007:18-38.
[7]	徐树宝,胡见义,李晋超,等.中俄土天然气地质研究新进展[M].北京:石油工业出版社,1995:126-137. Xu Shubao,Hu Jianyi,Li Jinchao,et al.China and Russia soil gas geological research progress[M].Beijing:Petroleum Industry Press,1995:126-137.
[8]	方杰,徐树宝,吴蕾,等.阿姆河右岸地区侏罗系海相烃源岩生烃潜力[J].海相油气地质,2014,19(1):8-18. Fang Jie,Xu Shubao,Wu Lei,et al.Hydrocarbon generation potential of Jurassic source rocks in right bank of Amu Darya[J].Marine Origin Petroleum Geology,2014,19(1):8-18.
[9]	白国平,殷进垠.中亚卡拉库姆盆地油气分布特征与成藏模式[J].古地理学报,2007,9(3):293-301. Bai Guoping,Yin Jinyin.Distribution characteristics and accumulation model for oil and gas in Karakum Basin, Central Asia[J].Journal of Palaeogeography,2007,9(3):293-301.
[10]	聂明龙,吴蕾,孙林,等.阿姆河盆地查尔朱阶地及邻区盐相关断裂特征与油气地质意义[J].石油与天然气地质,2012,34(6):803-808. Nie Minglong,Wu Lei,Sun Lin,et al.Salt-related fault characteristics and their petroleum geological significance in Zarzhu terrace and its adjacent areas,the Amu Darya Basin[J].Oil & Gas Geology,2012,34(6):803-808.
[11]	Zheng Rongcai,Li Yun,Wu Lei,et al.Geochemical characteristics of Callovian-Oxfordian carbonates in Samandepe gas field,Amu Darya Basin,Turkmenistan[J].Petroleum Science,2011,8(4):371-381]
[12]	郑荣才,陈浩如,王强,等.土库曼斯坦阿姆河盆地卡洛夫-牛津阶储层特征及控制因素分析[J].岩石学报,2014,30(3):779-788. Zheng Rongcai,Chen Haoru,Wang Qiang,et al.The reservoir characteristics and their controlling factors of Callovian-Oxfor-dian carbonates in Amu Darya Basin[J].Acta Petrologica Sinica,2014,30(3):779-788.
[13]	徐文礼,郑荣才,费怀义,等.土库曼斯坦阿姆河盆地卡洛夫-牛津阶沉积相特征[J].中国地质,2012,39(4):954-964. Xu Wenli,Zheng Rongcai,Fei Huaiyi,et al.The sedimentary facies of Callovian-Oxfordian Stage in Amu Darya basin,Turk-menistan[J].Geology in China,2012,39(4):954-964.
[14]	张兵,郑荣才,刘合年,等.土库曼斯坦萨曼杰佩气田卡洛夫阶-牛津阶碳酸盐岩储层特征[J].地质学报,2010,84(1):117-126. Zhang Bing,Zheng Rongcai,Liu Henian,et al.Characteristics of carbonate reservoir in Callovian-Oxfordian of Samandepe Gasfield,Turkmenistan[J].Acta Geologica Sinica,2010,84(1):117-126.
[15]	Robert A M M,Letouzey J,Kavoosi M A,et al.Structural evolution of the Kopeh Dagh fold-and-thrust belt (NE Iran) and interactions with the South Caspian Sea Basin and Amu Darya Basin[J].Marine and Petroleum Geology,2014,57:68-87.
[16]	徐文世,刘秀联,余志清,等.中亚阿姆河含油气盆地构造特征[J].天然气地球科学,2009,20(5):744-748. Xu Wenshi,Liu Xiulian,Yu Zhiqing,et al.Geological structure of Amu-Darya Basin in central Asia[J].Natural Gas Geoscience,2009,20(5):744-748.
[17]	张志伟,何永垚,王春生,等.中亚地区阿姆河盆地查尔朱、布哈拉阶地构造特征及演化[J].海相油气地质,2010,15(4):48-56. Zhang Zhiwei,He Yongyao,Wang Chunsheng,et al.Structural characteristics and evolution of Chardzhou and Bukhara Terraces in Amu-Darya Basin,middle Asia[J].Marine Origin Petroleum Geology,2010,15(4):48-56.
[18]	聂明龙,吴蕾,徐树宝,等.阿姆河盆地别什肯特坳陷及其邻区构造成因与勘探意义[J].天然气工业,2013,33(11):45-50. Nie Minglong,Wu Lei,Xu Shubao,et al.Genetic mechanism and exploration significance of tectonic action in the Bieshikent Depre-ssion and its adjacent area in the Amu-Darya Basin[J].Natural Gas Industry,2013,33(11):45-50.