松辽盆地北部油页岩资源潜力评价

doi:10.13278/j.cnki.jjuese.201503103

摘要/Abstract

摘要：

为评价松辽盆地北部油页岩资源潜力,开展了14口地质井的钻探、2 100多口老井的复查和多项油页岩的样品分析测试工作。根据油页岩分析测试资料,结合录井、测井、地震、沉积等研究成果,总结了油页岩主要特征,并用体积丰度法初步估算了埋深小于1 km的油页岩和页岩油潜在资源量。结果表明:松辽盆地北部油页岩主要发育在青山口组一段和嫩江组一、二段沉积时期的湖相沉积中,是盆地两次最大湖泛期的产物;嫩江组和青山口组油页岩平均岩石密度分别为2.20和2.18 t/m³,平均含油率分别为5.55%和5.39%;油页岩有机质类型为Ⅰ型和Ⅱ₁型,处于未成熟低成熟阶段,有机质丰度极高,是最好的生油岩。松辽盆地北部油页岩分布广泛、层位稳定、资源潜力巨大,初步估算埋深小于1 km的油页岩潜在资源量为6 008.40×10⁸ t,页岩油潜在资源量为297.50×10⁸ t。油页岩可以成为未来大庆油田常规油气的重要补充或接替资源。

关键词: 松辽盆地, 油页岩, 含油率, 沉积环境, 地球化学, 资源潜力

Abstract:

In order to evaluate the oil shale resource potential in north Songliao basin, 14 geological wells are drilled, more than 2 100 old wells are reviewed and a number of oil shale samples are tested. According to the testing data of the oil shale, combined with the well logging, seismic, deposit, and the other research achievements, the main characteristics of oil shale is summarized, and the potential resources of oil shale and shale oil,buried less than 1 000 m in depth, are preliminarily estimated using the volume abundance method. Oil shales in north Songliao basin are mainly developed in the lacustrine deposit when the first section of Qingshankou Formation, the first and second section of Nenjiang Formation deposited, which are the results of the twice maximum flooding period in the basin. The average density of oil shale in Nenjiang Formation and Qingshankou Formation is 2.20 t/m³ and 2.18 t/m³ respectively, and the average oil yield is 5.39% and 5.55% respectively. The types of organic matter of the oil shale are I and II₁ in the developing stage from immaturity to low maturity; and they are excellent hydrocarbon source rocks. Oil shale resources in north Songliao basin are widely distributed, stable in strata, and have a great resource potential. It is estimated that the potential resource of oil shale is 6 008.40×10⁸ t and of shale oil is 297.50×10⁸ t for those are buried less than 1 000 m in depth. The oil shale can be an important supplement or replacement of the conventional oil and gas in Daqing oil field in the near future.

Key words: Songliao basin, oil shale, oil yield, depositional environment, geochemistry, resource potential

中图分类号:

P618.12

郑玉龙, 陈春瑞, 王佰长, 王占国, 刘胜英, 吴相梅. 松辽盆地北部油页岩资源潜力评价[J]. 吉林大学学报(地球科学版), 2015, 45(3): 683-690.

Zheng Yulong, Chen Chunrui, Wang Baichang, Wang Zhanguo, Liu Shengying, Wu Xiangmei. Resource Potential Evaluation of Oil Shale in North Songliao Basin[J]. Journal of Jilin University(Earth Science Edition), 2015, 45(3): 683-690.

参考文献

[1] 钱家麟,尹亮. 油页岩:石油的补充能源[M]. 北京:中国石化出版社,2008. Qian Jialin, Yin Liang. Oil Shale:Complement Resources of Oil[M]. Beijing: Petroleum Industrial Press, 2008.

[2] 刘招君,董清水,叶松青,等. 中国油页岩资源现状[J]. 吉林大学学报: 地球科学版,2006,36(6):869-876. Liu Zhaojun, Dong Qingshui, Ye Songqing, et al. The Situation of Oil Shale Resources in China[J]. Journal of Jilin University: Earth Science Edition, 2006,36(6):869-876.

[3] 刘招君,杨虎林,董清水,等. 中国油页岩[M]. 北京:石油工业出版社,2009. Liu Zhaojun, Yang Hulin, Dong Qingshui, et al. Oil Shale in China[M]. Beijing: Petroleum Industrial Press, 2009.

[4] 隋军,梁文福,冀宝发. 不断创新开发技术,支撑大庆油田持续稳产[J]. 大庆石油地质与开发,2009,28(5):64-68. Sui Jun, Liang Wenfu, Ji Baofa. Based on Continuous Innovation of Development Technology to Achieve Sustainable Production in Daqing Oilfield[J]. Petroleum Geology and Oilfield Development in Daqing,2009,28(5):64-68.

[5] 冯志强. 技术进步是油气勘探持续发展的不竭动力[J]. 大庆石油地质与开发,2009,28(5):6-12. Feng Zhiqiang. Technical Progress Provides Inexhaustible Power for the Sustainable Development of Hydrocarbon Exploration[J]. Petroleum Geology and Oilfield Development in Daqing,2009,28(5):6-12.

[6] 大庆油田石油地质志编写组.中国石油地质志:卷二:大庆、吉林油田:上册:大庆油田[M]. 北京:石油工业出版社,1993. Writing Group of Daqing Oilfield Petroleum Geology. Petroleum Geology of China:Vol 2:Daqing, Jilin Oil Field:Vol 1:Daqing Oil Field[M]. Beijing: Petroleum Industrial Press, 1993.

[7] 叶得泉,黄清华,张莹,等. 松辽盆地白垩纪介形类生物地层学[M]. 北京:石油工业出版社,2002. Ye Dequan, Huang Qinghua, Zhang Ying, et al. Cretaceous Ostracoda Biostratigraphy in Songliao Basin[M]. Beijing: Petroleum Industrial Press, 2002.

[8] 侯读杰,冯子辉,黄清华. 松辽盆地白垩纪缺氧地质事件的地质地球化学特征[J]. 现代地质,2003,17(3):311-317. Hou Dujie, Feng Zihui, Huang Qinghua. Geological and Geochemical Evidences of Anoxic Event in the Songliao Basin, China[J]. Geoscience,2003,17(3):311-317.

[9] 陈雪凝,陆永潮,吴河勇. 白垩纪大洋沉积转变期间松辽盆地的沉积响应[J]. 天然气勘探与开发,2007,30(3):32-36. Chen Xuening, Lu Yongchao, Wu Heyong. Sedimentary Response of Songliao Basin During Cretaceous Oceanic Depositional Transition[J]. Natural Gas Exploration and Development,2007,30(3):32-36.

[10] 高瑞祺,张莹,崔同翠. 松辽盆地白垩纪石油地层[M]. 北京:石油工业出版社,1994. Gao Ruiqi, Zhang Ying, Cui Tongcui. Cretaceous Oil and Gas Strata of Songliao Basin[M]. Beijing: Petroleum Industrial Press, 1994.

[11] SY/T5735-1995 陆相烃源岩地球化学评价方法[S]. 北京:石油工业出版社,1996. SY/T5735-1995 Continental Source Rock Geochemical Evaluation Method[S]. Beijing: Petroleum Industrial Press, 1996.

[12] 刘振文,王佰长,郑玉龙,等. 黑龙江省柳树河盆地五林勘查区油页岩特征[J]. 大庆石油地质与开发,2010,29(6):34-38. Liu Zhenwen, Wang Baichang, Zheng Yulong, et al. Characteristics of Oil Shale in Wulin Prospecting Area in Liushuhe Basin, Heilongjiang Province[J]. Petroleum Geology and Oilfield Development in Daqing,2010,29(6):34-38.

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