塔里木盆地石炭系卡拉沙依组烃源岩研究

李京昌; 吴疆; 何宏; 许杰; 郭忻

doi:10.11781/sysydz201704511

塔里木盆地石炭系卡拉沙依组烃源岩研究

doi: 10.11781/sysydz201704511

李京昌¹,
吴疆¹,
何宏¹,
许杰¹,
郭忻²

1.
中国石化石油勘探开发研究院, 北京 100083
2. 中国石化西北油田分公司石油勘探开发研究院, 乌鲁木齐 830011

基金项目: 中国石化科技部项目“塔里木盆地中石化登记区块基础石油地质研究与综合评价”（34400008-17-ZC0607-0001）资助。

详细信息

作者简介:
李京昌(1965—),男,高级工程师,从事含油气盆地分析研究。E-mail:lijc.syky@sinopec.com。

中图分类号: TE122.112
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出版历程
- 收稿日期: 2016-08-09
- 修回日期: 2017-06-03
- 刊出日期: 2017-07-28

Source rock characteristics of the Carboniferous Karashayi Formation in the Tarim Basin

1.
SINOPEC Petroleum Exploration and Production Research Institute, Beijing 100083, China
2. Institute of Petroleum Exploration and Production, SINOPEC Northwest Oilfield Company, Urumqi, Xinjiang 830011, China

摘要

摘要: 为了进一步搞清楚塔里木盆地石炭系各个层系烃源岩发育的规模，达到对石炭系烃源岩深入研究的目的，对石炭系卡拉沙依组碎屑岩开展了有机质丰度、厚度、分布范围以及有机质类型和成熟度研究。结果表明，卡拉沙依组砂泥岩段发育的时期是卡拉沙依组优质烃源岩发育最重要阶段；卡拉沙依组砂泥岩段潟湖相分布的区域，即以玛参1井为中心的玛扎塔格构造带附近是优质烃源岩分布最好的区域，甚至优于塔西南山前带，在这一区域中有机碳含量大于2%，厚约60 m，处于低成熟-成熟的过渡阶段。但是，总体上看，塔里木盆地卡拉沙依组优质烃源岩分布相对局限。
- 烃源岩 /
- 卡拉沙依组 /
- 石炭系 /
- 塔里木盆地
Abstract: The organic matter abundance, thickness, distribution range, organic matter type and maturity of clastic rocks in the Carboniferous Karashayi Formation were studied in order to further clarify the scale of hydrocarbon source rocks in the Carboniferous strata in the Tarim Basin. The period when sandstones and mudstones were deposited in the Karashayi Formation was the most important period for the generation of high quality hydrocarbon source rocks. The lagoon facies area close to the Mazatage structural belt with Macan1 well at the center is the best area for high quality source rocks, even better than the southwestern Tarim Basin. Source rocks in this area are about 60 m thick, generally low mature or mature. The organic carbon content is greater than 2%. However, in general, the distribution of high quality source rocks in the Karasayi Formation of the Tarim Basin is relatively limited.
- source rock /
- Karashayi Formation /
- Carboniferous /
- Tarim Basin

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参考文献(25)

[1]	王君奇,武涛.塔里木盆地石炭系沉积特征及石油地质意义[J].石油实验地质,1999,21(1):23-27. Wang Junqi,Wu Tao.The Carboniferous depositional characteristics and petroleum geology in the Tarim Basin[J].Experimental Petroleum Geology,1999,21(1):23-27.
[2]	丁勇,宫继萍,王辉.塔里木盆地西南坳陷生油岩综合评价[J].石油实验地质,1999,21(4):336-339. Ding Yong,Gong Jiping,Wang Hui.Synthetic evaluation of source rocks in southwest depression of the Tarim Basin[J].Experimental Petroleum Geology,1999,21(4):336-339.
[3]	曾昌民,张亮,雷刚林,等.塔西南坳陷烃源岩生标特征对比及沉积环境指示意义[J].新疆地质,2011,29(3):319-323. Zeng Changmin,Zhang Liang,Lei Ganglin,et al.Biomarkers charac-teristics of source rocks of south-west Tarim depression and its signification for sedimentary environment[J].Xinjiang Geology,2011,29(3):319-323.
[4]	赵文智,张光亚.被动大陆边缘演化与油气地质:以塔里木盆地西南地区为例[M].北京:石油工业出版社,2007. Zhao Wenzhi,Zhang Guangya.Passive continental margin evolution and oil-gas geology:A case study of Tarim Basin[M].Beijing:Petroleum Industry Press,2007.
[5]	孟苗苗,康志宏,徐耀辉,等.塔里木盆地喀什凹陷烃源岩地球化学特征和油源对比[J].石油实验地质,2016,38(2):266-272. Meng Miaomiao,Kang Zhihong,Xu Yaohui,et al.Geochemical characteristics of source rocks and oil-source correlation in the Kashi Sag,Tarim Basin[J].Petroleum Geology & Experiment,2016,38(2):266-272.
[6]	吕海涛,顾忆,丁勇,等.塔里木盆地西南部皮山北新1井白垩系油气成因[J].石油实验地质,2016,38(1):84-90. Lü Haitao,Gu Yi,Ding Yong,et al.Cretaceous petroleum origin in well PSBX1 in the southwestern Tarim Basin[J].Petroleum Geology & Experiment,2016,38(1):84-90.
[7]	常健,邱楠生,刘一锋,等.塔里木盆地石炭系烃源岩成熟演化研究[J].地质科学,2014,49(3):823-841. Chang Jian,Qiu Nansheng,Liu Yifeng,et al.Maturity evolution of the Carboniferous source rocks(CSR) in the Tarim Basin,Northwest China[J].Chinese Journal of Geology,2014,49(3):823-841.
[8]	程顶胜,刘松,吴培红.塔里木盆地石炭系生烃潜力的模糊数学综合评价[J].石油学报,2000,21(1):34-39. Cheng Dingsheng,Liu Song,Wu Peihong.Comprehensive evaluation by fuzzy mathematics on hydrocarbon generation potential of carboniferous source rocks in Tarim Basin[J].Acta Petrolei Sinica,2000,21(1):34-39.
[9]	郭齐军,赵省民.塔河地区石炭系沉积特征[J].石油与天然气地质,2002,23(1):99-102. Guo Qijun,Zhao Xingmin.Depositional characteristics of carboni-ferous in Tahe region[J].Oil & Gas Geology,2002,23(1):99-102.
[10]	何发岐,翟晓先,俞仁连,等.塔河油田石炭系卡拉沙依组沉积与成因分析[J].石油与天然气地质,2004,25(3):258-262. He Faqi,Zhai Xiaoxian,Yu Renlian,et al.Deposition and genetic analysis of Carboniferous Kalashayi Formation in Tahe oilfield[J].Oil & Gas Geology,2004,25(3):258-262.
[11]	黄智斌,杜品德,张师本,等.塔里木盆地石炭系卡拉沙依组的厘定[J].地层学杂志,2005,29(1):55-61. Huang Zhibin,Du Pinde,Zhang Shiben,et al.Revision of the Carboniferous Kalashayi Formation of the Tarim Basin[J].Journal of Stratigraphy,2005,29(1):55-61.
[12]	张师本,黄智斌,朱怀诚.塔里木盆地覆盖区显生宙地层[M].北京:石油工业出版社,2004. Zhang Shiben,Huang Zhibin,Zhu Huaicheng.Phanerozoic strata in the coverage area of Tarim Basin[M].Beijing:Petroleum Industry Press,2004.
[13]	郭书元,詹伟,黄太柱,等.塔里木盆地石炭系划分对比及玛扎塔格组的建立[J].地层学杂志,2014,38(2):147-160. Guo Shuyuan,Zhan Wei,Huang Taizhu,et al.The Carboniferous stratigraphic division and correlation and a new lithostratigraphic unit:The Mazatage Formation in the Tarim Basin[J].Journal of Stratigraphy,2014,38(2):147-160.
[14]	许杰,郭建华,何治亮.塔里木盆地石炭系层序地层研究[J].海洋地质动态,2008,24(10):19-28. Xu Jie,Guo Jianhua,He Zhiliang.Sequence stratigraphy of the Carboniferous in Tarim Basin[J].Marine Geology Letters,2008,24(10):19-28.
[15]	许璟,蒲仁海,郭倩.塔里木盆地卡拉沙依组砂泥岩段地层对比与沉积相研究[J].特种油气藏,2012,19(4)：51-55. Xu Jing,Pu Renhai,Guo Qian.Stratigraphic correlation and sedimentary facies of the sandstone and mudstone section in the Kalashayi formation of Tarim Basin[J].Special Oil & Gas Reservoirs,2012,19(4)：51-55.
[16]	许璟,蒲仁海.卡拉沙依组砂泥岩段地震反演储层识别[J].特种油气藏,2014,21(2):61-65. Xu Jing,Pu Renhai.Reservoir identification by use of seismic inversion in the Kalashayi Formation arenaceous mudstone interval within the 3D area [J].Special Oil & Gas Reservoirs,2014,21(2):61-65.
[17]	盛湘,何发岐,云露.塔河地区卡拉沙依组小层划分、连通性及油藏类型[J].石油与天然气地质,2009,30(2):143-148. Sheng Xiang,He Faqi,Yun Lou.Subzone division,connectivity and pool types of the Carboniferous Kalashayi Formation in the Tahe area[J].Oil & Gas Geology,2009,30(2):143-148.
[18]	许杰,何治亮,郭建华,等.卡拉沙依组砂泥岩段层序地层及沉积体系[J].新疆地质,2009,27(2):155-159. Xu Jie,He Zhiliang,Guo Jianhua,et al.Sequence stratigraphy and sedimentry system of Kalashayi Formation sandy mudstone member[J].Xinjiang Geology,2009,27(2):155-159.
[19]	陈建平,梁狄刚,张水昌,等.中国古生界海相烃源岩生烃潜力评价标准与方法[J].地质学报,2012,86(7):1132-1142. Chen Jianping,Liang Digang,Zhang Shuichang,et al.Evaluation criterion and methods of the hydrocarbon generation potential for China's Paleozoic marine source rocks[J].Acta Geologica Sinica,2012,86(7):1132-1142.
[20]	柳广弟,孙明亮."石油地质学"课程研究性教学探索与实践[J].中国地质教育,2013,22(1):43-47. Liu Guangdi,Sun Mingliang.Exploration and practice of the research-based teaching of petroleum geology[J].Chinese Geological Education,2013,22(1):43-47.
[21]	夏新宇.碳酸盐岩生烃与长庆气田气源[M].北京:石油工业出版社,2000. Xia Xinyu.Hydrocarbon potential evaluation of carbonates and source rock correlation of the Changqing Gasfield[M].Beijing:Petroleum Industry Press,2000.
[22]	钟宁宁,卢双舫,黄志龙,等.烃源岩TOC值变化与其生排烃效率关系的探讨[J].沉积学报,2004,22(S1):73-78. Zhong Ningning,Lu Shuangfang,Huang Zhilong,et al.An approach to the evolution of TOC value for source rock and its relation to efficiencies of hydrocarbon generation and expulsion[J].Acta Sedimentologica Sinica,2004,22(S1):73-78.
[23]	程克明,王铁冠,钟宁宁.烃源岩地球化学[M].北京:科学出版社,1995. Cheng Keming,Wang Tieguan,Zhong Ningning.Geochemistry of source rocks[M].Beijing:Science Press,1995.
[24]	Tissot B P,Pelet R,Ungerer P.Thermal history of sedimentary basins,maturation indices,and kinetics of oil and gas generation[J].AAPG Bulletin,1987,71(12):1445-1466.
[25]	李贤庆,马安来,钟宁宁,等.烃源岩有机岩石学研究方法与应用[M].重庆:重庆大学出版社,1997. Li Xianqing,Ma Anlai,Zhong Ningning,et al.Research method and application of organic rock in source rock[M].Chongqing:Chongqing University Press,1997.