岩性油气藏 ›› 2021, Vol. 33 ›› Issue (1): 175–185.doi: 10.12108/yxyqc.20210116

• 油气地质 • 上一篇    下一篇

鄂博梁构造带油气成藏条件分析及勘探启示

孔红喜, 王远飞, 周飞, 朱军, 陈阳阳, 宋德康   

  1. 中国石油青海油田分公司勘探开发研究院, 甘肃 敦煌 736202
  • 收稿日期:2020-09-11 修回日期:2020-11-18 出版日期:2021-02-01 发布日期:2021-01-25
  • 第一作者:孔红喜(1967-),男,高级工程师,主要从事矿物岩石学、沉积储层、石油地质综合研究等方面的工作。地址:(736202)甘肃省敦煌市七里镇青海油田勘探开发研究院天然气勘探研究所。Email:khxqh@petrochina.com.cn。
  • 基金资助:
    国家油气专项“岩性地层油气藏区带、圈闭有效性评价预测技术”（编号：2017ZX05001-003）、国家科技重大专项“柴达木复杂构造区油气成藏、关键勘探技术与新领域目标优选”（编号：2016ZX05003006）和中国石油重大科技专项“柴达木盆地建设高原大油气田勘探开发关键技术研究与应用”（编号：2016E-0102）联合资助

Hydrocarbon accumulation conditions in Eboliang structural belt and its exploration implications

KONG Hongxi, WANG Yuanfei, ZHOU Fei, ZHU Jun, CHEN Yangyang, SONG Dekang   

  1. Research Institute of Exploration and Development, PetroChina Qinghai Oilfield Company, Dunhuang 736202, Gansu, China
  • Received:2020-09-11 Revised:2020-11-18 Online:2021-02-01 Published:2021-01-25

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摘要： 鄂博梁构造带各构造均钻有以古近系—新近系为目的层的探井，但含气丰度很低，一直未能实现勘探的实际突破，同时限于侏罗系烃源岩层埋深较大，成藏富集规律认识不清。近年来随着勘探程度的不断提高，多口探井钻达侏罗系地层，为进一步深入研究奠定了基础。通过对鄂博梁构造带烃源岩、天然气地球化学特征以及运聚条件的详细分析，开展了成藏条件的综合研究。结果表明：处于边缘地区的牛东鼻隆—鄂博梁Ⅰ号构造有机质丰度不高、成熟度很低，不具备大规模形成天然气的烃源岩条件。目前已发现的天然气为高成熟、过成熟的煤型气，来自凹陷中心形成的高成熟烃源岩，侏罗系顶面广泛分布的不整合与沟通源岩的断层是主要的输导途径。鄂博梁构造带进一步的勘探工作应选择凹陷中心烃源岩成熟度高的地区，目的层应尽可能贴近源岩。该研究成果为鄂博梁构造带进一步勘探指出了有利勘探地区。

关键词: 烃源岩, 天然气组分, 甲烷碳同位素, 输导条件, 成藏模式, 勘探方向, 鄂博梁构造带, 柴达木盆地

Abstract: Exploration wells have been drilled in each structure of Eboliang structural belt with Paleogene and Neogene as the target layer,but the gas abundance is very low,so actual exploration breakthrough has not been achieved. At the same time,due to the large buried depth of Jurassic source rocks,the accumulation and enrichment rules are not clear. In recent years,with the continuous improvement of exploration degree,many exploration wells have been drilled to Jurassic,which lays a foundation for further study. Based on the analysis of hydrocarbon source rocks,geochemical characteristics of natural gas and migration and accumulation conditions of Eboliang structural belt,a comprehensive study on hydrocarbon accumulation conditions was carried out. The results show that the organic matter abundance is not high and the maturity is very low in Niudong nose-shaped uplift and Eboliang No. 1 structure,so they do not have the source rock conditions for large-scale natural gas formation. At present,the discovered natural gas is highly mature and over mature coal type gas,which comes from the highly mature source rocks formed in the center of the depression. The unconformities widely developed on the top of Jurassic and the faults connecting the source rocks are the main transport channels. The area with high maturity of source rock in the center of depression should be selected for the next exploration in Eboliang structural belt,and the target layer should be as close as possible to the source rocks. The research results indicate favorable exploration areas for further exploration in Eboliang structural belt.

Key words: source rocks, natural gas components, carbon isotope of methane, transport conditions, accumulation model, exploration direction, Eboliang structure belt, Qaidam Basin

中图分类号: 

  • TE121.1
[1] 李月,胥凯,颜世永,等. 含油气盆地油气输导体系分析. 油气地质与采收率,2015,22(1):32-36. LI Y,XU K,YAN S Y,et al. Study on hydrocarbon carrier system in petroliferous basins. Petroleum Geology and Recovery Efficiency,2015,22(1):32-36.
[2] 袁玲,任新成,穆玉庆,等. 准噶尔盆地春风油田油气输导体系.新疆石油地质,2012,33(3):288-289. YUAN L,REN X C,MU Y Q,et al. Oil-gas transport system in Chunfeng Oilfield in Junggar Basin. Xinjiang Petroleum Geology, 2012,33(3):288-289.
[3] 李坤,赵锡奎,张小兵,等. 塔里木盆地阿克库勒凸起油气输导体系类型与演化.地质科学,2007,42(4):766-778. LI K,ZHAO X K,ZHANG X B,et al. Hydrocarbon migration pathway system types and evolution in the akekule rise,Tarim Basin. Chinese Journal of Geology,2007,42(4):766-778.
[4] 王有功,张艳会,付广,等.松辽盆地尚家油田油气输导体系及特征. 西安石油大学学报:自然科学版,2012,27(1):17-22. WANG Y G,ZHANG Y H,FU G,et al. Study on hydrocarbon migration pathway system of Shangjia oilfield in Songliao Basin and its characteristics. Journal of Xi'an Petroleum University (Natural Science Edition),2012,27(1):17-22.
[5] 高斌斌,徐耀辉,李可文. 柴达木盆地柴北缘侏罗系烃源岩特征分析. 长江大学学报(自然科学版),2014,11(2):21-23. GAO B B,XU Y H,LI KW. Characteristics of the Jurassic source rocks in the northern edge of Qaidam Basin. Journal of Yangtze University(Natural Science Edition),2014,11(2):21-23.
[6] 胡勇,刘平,曹海防. 柴北缘侏罗系烃源岩地球化学特征及其综合评价.大地构造与成矿学,2004,28(4):464-469. HU Y,LIU P,CAO H F. Geochemical characteristics and hydrocarbon generation capability of the Jurassic hydrocarbon source rock on the northern edge of Qaidam Basin. Geotectonica et Metallogenia,2004,28(4):464-469.
[7] 翟志伟,张永庶,杨红梅,等. 柴达木盆地北缘侏罗系有效烃源岩特征及油气聚集规律. 天然气工业,2013,33(9):36-42. ZHAI Z W,ZHANG Y S,YANG H M,et al. Characteristics of effective source rocks in the Jurassic and hydrocarbon accumulation patterns in the areas near the northern margin of the Qaidam Basin. Natural Gas Industry,2013,33(9):36-42.
[8] 潘星,黄成刚,景茜,等. 柴达木盆地鄂博梁Ⅲ 号地区N21储层特征. 石油地质与工程,2015,29(2):64-67. PAN X,HUANG C G,JING Q,et al. N21 reservoir characteristics of Eboliang-Ⅲ in Qaidam Basin. Petroleum Geology and Engineering, 2015,29(2):64-67.
[9] 陈吉,史基安,孙国强,等. 鄂博梁Ⅲ 号构造上、下油砂山组成岩作用及对孔隙影响. 兰州大学学报(自然科学版),2012, 48(6):1-7. CHEN J,SHI JA,SUN G Q,et al. Diagenesis of lower-upperYoushashan Formation and its impact on porosity in No. Ⅲ structure of Eboliang area. Journal of Lanzhou University(Natural Sciences), 2012,48(6):1-7.
[10] 王鹏,赵澄林. 柴达木盆地北缘地区第三系碎屑岩储层沉积相特征. 石油大学学报(自然科学版),2001,25(1):12-15. WANG P,ZHAO C L. Characteristics of Tertiary reservoir sedimentary facies in the northern part of Qaidam Basin. Journal of the University of Petroleum,China(Edition of Natural Science), 2001,25(1):12-15.
[11] 汤国民,罗群,庞雄奇,等. 柴北缘鄂博梁Ⅲ 号构造天然气成因类型及其成藏特征.新疆石油地质,2014,35(1):17-22. TANG G M,LUO Q,PANG X Q,et al. Genetic types and accumulation characteristics of natural gas in the third structure of Eboliang in the northern margin of Qaidam Basin. Xinjiang Petroleum Geology,2014,35(1):17-22.
[12] 岳鹏升,王平,郁东良,等. 柴达木盆地北缘下中侏罗统沉积特征及其石油地质意义.海洋地质前沿,2011,27(11):38-44. YUE P S,WANG P,YU D L,et al. Depositional characteristics of the early and middle Jurassic on the northern margin of Qaidam Basin and their implications for petroleum geology. Marine Geological Frontiers,2011,27(11):38-44.
[13] 马立协,陈新领,张敏,等. 柴北缘逆冲带侏罗系油气成藏主控因素分析.石油地质,2006(6):22-25. MA L X,CHEN X L,ZHANG M,et al. Analysis on main controlling factors of Jurassic oil-gas reservoir-forming in thrusting belt in northern margin of Qaidam Basin. Petroleum Geology, 2006(6):22-25.
[14] 王桂宏,谭彦虎,陈新领,等. 新生代柴达木盆地构造演化与油气勘探领域.中国石油勘探,2006,11(1):80-84. WANG G H,TAN Y H,CHEN X L,et al. Cenozoic tectonic evolution and oil/gas exploration field in Qaidam Basin. China Petroleum Exploration,2006,11(1):80-84.
[15] 戴俊生,叶兴树,汤良杰,等. 柴达木盆地构造分区及其油气远景. 地质科学,2003,38(3):413-424. DAI J S,YE X S,TANG L J,et al. Tectonic units and oil-gas potential of Qaidam Basin. Chinese Journal of Geology,2003, 38(3):413-424.
[16] 赵凡,孙德强,闫存凤,等. 柴达木盆地中新生代构造演化及其与油气成藏关系.天然气地球科学,2013,24(5):940-947. ZHAO F,SUN D Q,YAN C F,et al. Meso-Cenozoic tectonic evolution of Qaidam Basin and its relationship with oil and gas accumulation. Natural Gas Geoscience,2013,24(5):940-947.
[17] 金之钧,张明利,汤良杰,等. 柴达木中新生代盆地演化及其控油气作用.石油与天然气地质,2004,25(6):603-608. JIN Z J,ZHANG M L,TANG L J,et al. Evolution of Meso-Cenozoic Qaidam Basin and its control on oil and gas. Oil & Gas Geology,2004,25(6):603-608.
[18] 方世虎,赵孟军,张水昌,等. 柴达木盆地北缘构造控藏特征与油气勘探方向. 地学前缘,2013,20(5):132-138. FANG S H,ZHAO M J,ZHANG S C,et al. Structural control on hydrocarbon accumulation and its implication for petroleum exploration in northern Qaidam Basin. Earth Science Frontiers,2013, 20(5):132-138.
[19] 周建勋,徐凤银,胡勇. 柴达木盆地北缘中、新生代构造变形及其对油气成藏的控制.石油学报,2003,24(1):19-24. ZHOU J X,XU F Y,HU Y. Mesozoic and Cenozoic tectonism and its control on hydrocarbon accumulation in the northern Qaidam Basin of China. Acta Petrolei Sinica,2003,24(1):19-24.
[20] 李明义,岳湘安,江青春,等.柴达木盆地北缘主要构造带构造演化与油气成藏关系.天然气地球科学,2012,23(3):461-468. LI M Y,YUE X A,JIANG Q C,et al. Relationship between hydrocarbon accumulation and tectonic evolution in main structural belt of the northern border of Qaidam Basin. Natural Gas Geoscience, 2012,23(3):461-468.
[21] 陈迎宾,胡烨,王彦青,等. 柴达木盆地鄂博梁Ⅲ 号构造深层天然气成藏条件. 油气地质与采收率.2013,24(5):940-947. CHEN Y B,HU Y,WANG Y Q,et al. Research on the deep gas accumulation conditions of Eboliang-Ⅲ structure,Qaidam Basin. PetroleumGeology and Recovery Efficiency,2013,24(5):940-947.
[22] 于会娟,妥进才,刘洛夫,等. 柴达木盆地东部地区侏罗系烃源岩地球化学特征及生烃潜力评价. 沉积学报,2000,18(1):132-138. YU H J,TUO J C,LIU L F,et al. Geochemical characteristics and hydrocarbon generation potential of Jurassic source. Acta Sedimentologica Sinica,2000,18(1):132-138.
[23] 陈艳鹏,刘震,李潍莲,等.柴达木盆地油气成藏构造演化作用浅析. 西南石油大学学报(自然科学版),2008,30(4):43-47. CHEN Y P,LIU Z,LI W L,et al. Tectonic evolution and formation of reservoirs in Qaidam Basin. Journal of Southwest Petroleum University(Science & Technology Edition),2008,30(4):43-47.
[24] 徐凤银,彭德华,侯恩科,等. 柴达木盆地油气聚集规律及勘探前景. 石油学报,2003,24(4):1-6. XU F Y,PENG D H,HOU E K,et al. Hydrocarbon accumulation and exploration potential in Qaidam Basin. Acta Petrolei Sinica, 2003,24(4):1-6.
[25] 付小东,饶丹,秦建中,等.柴达木盆地北缘地区中侏罗统大煤沟组页岩油形成地质条件. 岩性油气藏,2014,26(6):20-27. FU X D,RAO D,QIN J Z,et al. Geological conditions of shale oil formation of Middle Jurassic Dameigou Formation in northern margin of Qaidam Basin. Lithologic Reservoirs,2014,26(6):20-27.
[26] 曾花森,蔡郁文,霍秋立,等. 烃源岩中有效有机质的类型评价及意义.大庆石油地质与开发,2013,32(3):8-14. ZENG H S,CAI YW,HUO Q L,et al. Evaluation of the effective organic matter types in hydrocarbon source rock and its implication. Petroleum Geology & Oilfield Development in Daqing, 2013,32(3):8-14.
[27] 祁帅,李贤庆,何坤,等. 不同类型有机质热演化轻烃产率及组成特征对比.天然气地球科学,2017,28(6):975-986. QI S,LI X Q,HE K,et al. Comparative research on the yields and chemical compositions of light hydrocarbons derived from pyrolysis of organic matters with different types. Natural Gas Geoscience,2017,28(6):975-986.
[28] 戴金星,龚剑明. 中国煤成气理论形成过程及对天然气工业发展的战略意义,中国石油勘探,2018,23(4):1-10. DAI J X,GONG JM. Establishment of coal-derived gas geological theory and its strategic significance to the development of natural gas industry in China. China Petroleum Exploration,2018, 23(4):1-10.
[29] 戴金星. 煤成气及鉴别理论研究进展. 科学通报,2018,63(14):44-59. DAI J X. Research progress of coal-derived gas and identification theory. Chinese Science Bulletin,2018,63(14):44-59.
[30] 宋成鹏,张晓宝,汪立群,等. 柴达木盆地北缘天然气成因类型及气源判识.石油与天然气地质,2009,30(1):90-96. SONG C P,ZHANG X B,WANG L Q,et al. A study on genetic types and source discrimination of natural gas in the north margin of the Qaidam Basin. Oil & Gas Geology,2009,30(1):90-96.
[31] 邢蓝田,张晓宝,张瑞,等. 柴北缘侏罗系烃源岩生烃动力学及其应用:以赛什腾凹陷为例,天然气地球科学,2012,23(1):161-166. XING L T,ZHANG X B,ZHANG R,et al. Kinetics of hydrocarbon generation for Jurassic source rochks and application in northern Qaidam Basin:Take Saishenteng Depression as an example. Natural Gas Geoscience,2012,23(1):161-166.
[32] 罗晓容,孙盈,汪立群,等. 柴达木盆地北缘西段油气成藏动力学研究.石油勘探与开发,2013,40(2):159-170. LUO X R,SUN Y,WANG L Q,et al. Dynamics of hydrocarbon accumulation in the west section of the northern margin of the Qaidam Basin,NWChina. Petroleum Exploration and Development, 2013,40(2):159-170.
[33] 曹正林,魏志福,张小军,等. 柴达木盆地东坪地区油气源对比分析. 岩性油气藏,2013,25(3):17-20. CAO Z L,WEI Z F,ZHANG X J,et al. Comparative analysis of oil and gas sources in Dongping area of Qaidam Basin. Lithologic Reservoirs,2013,25(3):17-20.
[34] 包建平,吴浩,朱翠山,等. 柴达木盆地北缘牛东地区煤成油及其地球化学特征.地质学报,2018,92(5):172-185. BAO J P,WU H,ZHU C S,et al. Coal-derived oil and the geochemical characteristics in the Niudong area,Qaidam Basin. Acta Geologica Sinica,2018,92(5):172-185.
[35] 包建平,王志峰,朱翠山,等. 柴达木盆地东坪地区一类新的原油及其地球化学特征.沉积学报,2018,36(4):829-841. BAO J P,WANG Z F,ZHU C S,et al.Anew kind of crude oils and the geochemical characteristics in the Dongping area,Qaidam Basin. Acta Sedimentologica Sinica,2018,36(4):829-841.
[36] 张景廉,石兰亭,陈启林,等. 柴达木盆地地壳深部构造特征及油气勘探新领域.岩性油气藏,2008,20(2):29-36. ZHANG J L,SHI L T,CHEN Q L,et al. Structural characteristics of deep crust and new areas of oil and gas exploration in Qaidam Basin. Lithologic Reservoirs,2008,20(2):29-36.
[37] 孙平,汪立群,郭泽清,等. 柴北缘鄂博梁构造带油气成藏条件及勘探部署.中国石油勘探,2014,19(4):18-25. SUN P,WANG L Q,GUO Z Q,et al. Oil and gas accumulation conditions of Eboliang structural belt on northern periphery of Qaidam Basin and exploration strategy. China Petroleum Exploration,2014,19(4):18-25.
[38] 孔红喜,赵健,侯泽生,等. 柴达木盆地鄂博梁Ⅲ 号构造新近系沉积环境演化及物源分析.古地理学报,2015,17(1):51-62. KONG H X,ZHAO J,HOU Z S,et al. Provenance analysis and sedimentary environment evolution of the Neogene in Eboliang Ⅲ structure of Qaidam Basin. Journal of Palaeogeography,2015, 17(1):51-62.
[39] 胡受权,郭文平,曹运江,等. 柴达木盆地北缘构造格局及在中、新生代的演化. 新疆石油地质,2001,22(1):13-16. HU S Q,GUOWP,CAOYJ,et al. Tectonic framework and structure evolution of Mesozoic and Cenozoic in northern margin of Qaidam Basin. Xinjiang Petroleum Geology,2001,22(1):13-16.
[40] 孙国强,杜忠明,贾艳艳,等. 柴达木盆地北缘西段古近纪以来沉积模式研究. 岩性油气藏,2012,24(4):13-18. SUN G Q,DU Z M,JIA Y Y,et al. Sedimentary model of the western segment of the northern margin of Qaidam Basin since Paleogene. Lithologic Reservoirs,2012,24(4):13-18.
[41] 林洪,郑兵. 柴达木盆地北缘鄂博梁地区新近系沉积相特征. 地层学杂志,2016,40(1):57-62. LIN H,ZHENG B. Tectonic framework and structure evolution of Mesozoic and Cenozoic in northern margin of Qaidam Basin. Journal of Stratigraphy,2016,40(1):57-62.
[42] 李俊武,杨承锦,李凤杰,等. 柴达木盆地鄂博梁地区新近系物源分析.古地理学报,2015,17(2):186-197. LI J W,YANG C J,LI F J,et al. The heavy minerals characteristics and provenance analysis of the Neogene in north margin of Qaidam Basin. Journal of Palaeogeography,2015,17(2):186-197.
[43] 李俊武,代廷勇,杜凌春,等. 柴北缘鄂博梁Ⅲ 号构造N1-N22砂岩储层孔隙特征及影响因素. 石油化工应用,2015,34(9):101-107. LI J W,DAI T Y,DU L C,et al. Characteristics of sandstone reservoir pore structure and its affecting factors analysis of the N1-N22 reservoir in Eboliang No. Ⅲ structure,Qaidam Basin. Petrochemical Industry Application,2015,34(9):101-107.
[44] 范昌育,王震亮,王爱国,等. 柴达木盆地北缘鄂博梁构造带超压形成机制与高压气、水层成因. 石油学报,2015,36(6):699-706. FANG C Y,WANG Z L,WANG A G,et al. Mechanisms for over pressure generation and origin of over pressured gas and aquifer layers,Eboliang structure belt,northern Qaidam Basin. Acta Petrolei Sinica,2015,36(6):699-706.
[45] 付锁堂,王震亮,张永庶,等. 柴北缘西段鄂博梁构造带储层碳酸盐胶结物成因及其油气地质意义:来自碳、氧同位素的约束. 沉积学报,2015,33(5):991-999. FU S T,WANG Z L,ZHANG Y S,et al. Origin of carbonate cements in reservoir rocks and its petroleum geologic significance:Eboliang structure belt,northern margin of Qaidam Basin. Acta Sedimentologica Sinica,2015,33(5):991-999.
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