塔里木盆地西北缘上震旦统微生物碳酸盐岩储层特征与成因

doi:10.11743/ogg20150310

摘要/Abstract

摘要： 通过野外露头地质观察、薄片鉴定与孔渗分析等，详细研究了塔里木盆地西北缘什艾日克剖面上震旦统微生物碳酸盐岩岩石学和储层特征，并简要分析了储层成因。研究认为该区上震旦统微生物碳酸盐岩以微生物白云岩为主，约占整个上震旦统碳酸盐岩的70.37%。根据是否具有叠层构造，将该区上震旦统微生物岩划分为叠层石和非叠层石两大类型，其中，叠层石类包括层状叠层石、丘状叠层石和小型孤立柱状叠层石，并以层状叠层石为主，结构以纹层球粒、泥晶为特征;而非叠层石包括非叠层蓝细菌球粒岩和非叠层蓝细菌泡沫绵层岩，结构以球粒、泡沫绵层为特征。根据储集性，可将该区上震旦统微生物岩储层划分为上、下两段，上段储层要优于下段。层状叠层石和非叠层蓝细菌球粒、泡沫绵层白云岩为有利储集岩石类型。微生物结构、白云石化和溶蚀作用为微生物岩储层形成的有利因素，其中微生物结构是基础，决定着微生物岩储层的孔隙类型及其孔隙结构特征，而白云石化和溶蚀作用则为微生物岩储层有效孔隙形成的关键因素，上段储层较好更得益于表生岩溶作用的影响。

关键词: 微生物, 碳酸盐岩储层, 上震旦统, 塔里木盆地

Abstract: Through outcrop observation, thin section examination and physical property analysis, this paper studied the petrological and reservoir characteristics of the Upper Sinian microbial carbonates on the Shiairike section at the northwestern margin of the Tarim Basin and briefly discussed the origin of the microbial carbonate reservoirs.The microbial carbonates are dominated by microbial dolomites, accounting for 70.37% of the whole Sinian carbonates.Based on having stromatilithic structure or not, the microbial carbonates are divided into stromatolites and non-stromatolites.The stomatolites include stratiform, domal and small isolate columnar types, with the stratiform stromatolites as the main type and pelletoid and micritic lamination as their texture characteristics.In contrast, the non-stromatolites include non-stromatolic cynobactiarial pellet rock and cyanobacterial foam spongy rock, featuring in pelletoid and foam sponge textures.According to physical property, the Sinian microbial carbonate reservoir can be divided into two intervals, with the upper interval being better than the lower.Among the microbial carbonates, the stratiform stromatolites and non-stromatolitic cyanobacterial dolostones especially with foam sponge-like texture are the favorable reservoir rocks.The reservoirs are characterized by fenestal, pellet-associated, foam sponge-associated dissolved porosity as their main reservoir space.The formation and distribution of the microbial carbonate reservoirs are mainly controlled by microfabrics, dolomatization and dissolution.Of these influencing factors, the microfabicsisthe fundamental factor determining the types of the pore space and their texture;the dolomization and dissolution are the critical factors determining the formation of effective pore space.The higher quality of the upper microbial carbonate reservoirs is also attributed to the epigenetic kastification.

Key words: microbial, carboante reservoir, Upper Sinian, Tarim Basin

中图分类号:

TE122.2

李朋威,罗平,陈敏,等. 塔里木盆地西北缘上震旦统微生物碳酸盐岩储层特征与成因[J]. 石油与天然气地质, 2015, 36(3): 416-428. doi: 10.11743/ogg20150310 Li Pengwei,Luo Ping,Chen Min,et al. Characteristics and origin of the Upper Sinian microbial carbonate reservoirs at the northwestern margin of Tarim Basin[J]. Oil & Gas Geology, 2015, 36(3): 416-428. doi: 10.11743/ogg20150310

参考文献

[1] Riding R.Microbial carbonates:the geological record of calcified bacterial-algal mats and biofilms[J].Sedimentology, 2000, 47(Suppl.1):179-214.
[2] James N P, Dalrymple R W.Facies and models[M].Library and Archives Canada Cataloguing in Publication, Geological Association of Canada, 2010.
[3] 杨浩, 王永标, 陈林, 等.地球微生物过程与潜在烃源岩的形成:钙质微生物岩[J].地球科学——中国地质大学学报, 2007, 32(6):797-802. Yang H, Wang Y B, Chen L, et al.Calci-M icrobialite as a kind of potential hydrocarbon source rock and its geomicrobiological processes[J].Earth Science:Journal of China University of Geosciences, 2007, 32(6):797-802.
[4] 李朋威, 金廷福, 王果谦, 等.微生物碳酸盐岩及其油气勘探意义[J].地质科技情报, 2013, 32(3):66-74. Li Pengwei, Jin Tingfu, Wang Guoqian, et al.Microbial carbonates and their significance in the petroleum exploration[J].Geological Science and Technology Information, 2013, 32(3):66-74.
[5] Mancini E A, Benson D J, Hart B S, et al.Appleton field case study (eastern Gulf coastal plain):Field development model for Upper Jurassic microbial reef reservoirs associated with paleotopographic basement structures[J].AAPG Bulletin, 2000, 84(11):1699-1717.
[6] Mancini E A, Llina's J C, Parcell W C, et al.Upper Jurassic throm-bolite reservoir play, northeastern Gulf of Mexico[J].AAPG Bulletin, 2004, 88(11):1573-1602.
[7] 李国玉.从东西伯利亚古老地层看中国震旦系含油气前景[J].海相油气地质, 2006, 11(3):1-3. Li Guoyu.The petroleum propects of the Sinian system in China speculated from the Eastern Siberian old strata[J].Marin Origin Petroleum Geology, 2006, 11(3):1-3.
[8] Wright P V, Racey A.Pre-salt microbial carbonate reservoirs of the santos Basin, offshore Brazil.AAPG Annual Convention and Exhibition, Colorado Convention Center, 2009.
[9] Grotzinger J P, Amthor J E.Facies and reservoir architecture of isolated microbial carbonate platforms, terminal Proterozoic-early Cambrian Ara Group, South Oman Salt Basin.AAPG Annual Meeting, Houston, Texas, 2002.
[10] Schröder S, Grotzinge J P, Amthor J E, et al.Carbonate deposition and hydrocarbon reservoir development at the Precambrian-Cambrian boundary:The Ara Group in South Oman[J].Sedimentary Geology, 2005, 180:1-28.
[11] Kenter J A M, Harris P M M, Porta G D, et al.Microbial and cement boundstone-dominated flanks (and reservoirs) of an isolated carbonate platform.AAPG Annual Convention, Dallas, Texas, 2004.
[12] Kenter J A M, Harris P M M, Porta G D.Steep microbial boundstone-dominated platform margins-examples and implications[J].Sedimentary Geology, 2005, 178:5-30.
[13] 王兴志, 侯方浩, 黄继祥, 等.四川资阳地区灯影组储层的形成与演化[J].矿物岩石, 1997, 17(2):55-60. Wang Xingzhi, Hou Fanghao, Huang Jixiang, et al.The formation and evolution of reservoir in Sinian Dengying Formation, Ziyang Area, Sichuan Basin[J].Journal of Mineral Petrology , 1997, 17(2):55-60.
[14] 王兴志, 刘仲宣.影响四川资阳地区震旦系灯影组储集空间的主要因素[M].沉积学及岩相古地理学研究进展.石油工业出版社, 1995. Wang Xingzhi, Liu Zhongxuan.Influencing factors of the reservoir pore space in Sinian Dengying Formation, Ziyang area, Sichuan[M].Progress of Sedimentolgy and Lithofacies paleogeography, Petroleum Industrial Press, 1995.
[15] 余家仁, 樊哲仁.任丘古潜山油田碳酸盐岩储层研究[J].石油学报, 1981, 2(1):57-70. Yu Jiaren, Fan Zheren.A study on the carbonate reservoir rocks of Renqiu Buried-hill oilfield[J].Acta Petrolei Sinica, 1981, 2(1):57-70.
[16] 余家仁, 雷怀玉, 刘趁花.试论海相碳酸盐岩储层发育的影响因素——以任丘油田雾迷山组为例[J].海相油气地质, 1998, 3(1):39-48. Yu Jiaren, Lei Huaiyu, Liu Zhenhua.A discussion of factors influcing marine carbonate reservoir development:A case study of Wumishan Formation of Renqiu Oilfield[J].Marin Origin Petroleum Geology, 1998, 3(1):39-48.
[17] 罗平, 王石, 李朋威, 等.微生物碳酸盐岩油气储层研究现状与展望[J].沉积学报, 2013, 31(5):807-823. Luo Ping, Wang Shi, Li Pengwei, et al.Review and prospectives of microbial carbaonte reservoirs[J].acta Sedimentologica Snica, 2013, 31(5):807-823.
[18] 高振家, 王务严, 李永安, 等.新疆阿克苏-乌什震旦系[M].乌鲁木齐:新疆人民出版社, 1985. Gao Zhenjia, Wang Wushi, Li Yong'an, et al.The Sinian of Aksu-Wushi, XinJiang[M].Urumuqi:XinJiang People's Press, 1985.
[19] 高振家, 王务严, 彭昌文, 等.新疆震旦系[M].乌鲁木齐:新疆人民出版社, 1985. Gao Zhenjia, Wang Wuyan, Peng Cangwen, et al.The Sinian systerm in Xinjiang[M].Uromuqi:Xinjiang People's Press, 1985.
[20] 高振家, 朱诚顺.新疆前寒武纪地质[M].乌鲁木齐:新疆人民出版社, 1984. Gao Zhenjia, Zhu Chengshun.The Precambrian, Xinjiang[M].Urumuqi:Xinjiang People's Press, 1984.
[21] 史基安.塔里木盆地西北缘震旦系和古生代白云岩成因及其储集性[J].沉积学报, 1993, 11(2):43-50. Shi Ji'an.The origin of dolostone and its reservoir characteristics of Sinian and Palaeozoic, northwestern margin of Tarim Basin[J].Acta Sedimentologica Sinica, 1993, 11(2):43-50.
[22] 王小林, 胡文暄, 陈奇, 等.塔里木盆地柯坪地区上震旦统藻白云岩特征及其成因机理[J].地质学报, 2010, 84(10):1479-1494. Wang Xiaolin, Hu Wenxuan, Chen Qi, et al.Characteristics and formation mechanism of Upper Sinian Algal dolomite at the Kalpin area, Tarim Basin, NW China[J].Acta Geologica Sinica, 2010, 84(10):1479-1494.
[23] 宋金民, 罗平, 杨式升, 等.塔里木盆地苏盖特布拉克地区下寒武统肖尔布拉克组碳酸盐岩微生物建造特征[J].古地理学报, 2012, 14(3):341-354. Song Jinmin, Luo Ping, Yang Shisheng et al.Carbonate rock microbial construction of the Lower Cambrian Xiaoerblak Fromation in Sugaitblak area, Tarim Basin[J].Journal of Palaeogeography, 2012, 14(3):341-354.
[24] 宋金民, 罗平, 杨式升, 等.苏盖特布拉克地区下寒武统微生物礁演化特征[J].新疆石油地质, 2012, 33(6):668-671. Song Jinmin, Luo Ping, Yang Shisheng, et al.Evolution characteristics of microbial reef of Lower Cambrian in Sugaiteblak area, Tarim Basin[J].Xinjiang Petroleum Geology, 2012, 33(6):668-671.
[25] 宋金民, 罗平, 杨式升, 等.塔里木盆地下寒武统微生物碳酸盐岩储集层特征[J].石油勘探与开发, 2014, 41(4):404-437. Song Jinmin, Luo Ping, Yang Shisheng, et al.Reservoirs of Lower Cambrian microbial carbonates, Tarim Basin, NW China[J].Petroleum Exploration and Development, 2014, 41(4):404-437.
[26] 胡文瑄, 朱井泉, 王小林等.塔里木盆地柯坪地区寒武系微生物白云岩特征、成因及意义[J].石油与天然气地质, 2014, 35(6):860-869. Hu Wenxuan, Zhu Jingquan, Wang Xiaolin et al.Characteristics, origin and geological implications of the Cambrian microbialdolomite in Keping area, Tarim Basin.Oil & Gas Geology, 2014, 35(6):860-869
[27] 由雪莲, 孙枢, 朱井泉, 等.微生物白云岩模式研究进展[J].地学前缘(中国地质大学(北京);北京大学), 2011, 18(4):52-64. You Xuelian, Sun Shu, Zhu Jingquan et al.Progress in the study of microbial dolomite model[J].Earth Science Frontiers(China University of Geosciences(Beijing);Peking University), 2011, 18(4):52-64.
[28] Riding, R.and Fan J.Ordovician calcified algae and cyanobacteria, northern Tarim Basin subsurface, China.Palaeontology, 2001, 44(3):783-810.
[29] 范嘉松, 吴亚生.从塔北隆起奥陶纪钙藻化石探讨奥陶纪的古环境[J].微体古生物学报, 2004.21(3):251-266. Fan Jiasong, Wu Yasheng.Palaeoenvironmental analysis of Ordovician rocks in the northern uplift of Tarim Basin in terms of calcareous algae and cyanobacteria[J].Acta Micropalaeontologica Sinica, 2004, 21(3):251-266.
[30] 王建坡, 李越, 张园园, 等.新疆巴楚晚奥陶世礁丘中的蓝菌群落[J].微体古生物学报, 2009.26(2):139-147. Wang Jianbo, Li Yue, Zhang Yuanyuan, et al.Cyanobacterial commnity from the reef mound of the Lianglitag Formation( Upper Ordovician), Bachu, Xinjiang, NW China[J].Acta Micropalaeontologica Sinica, 2009.26(2):139-147.
[31] 杨海军, 王建波, 黄智斌, 等.塔中隆起上奥陶统凯迪阶良里塔格组生物群及其古生态特征[J].古生物学报, 2009.8(1):109-122. Yang Haijun, Wang Jianbo, Huangzhibin et al.Biota and Palaeoecology of the Lianglitag Formation(Katian, Upper Ordovician), Central Tarim, NW China[J].Acta Palaeontologica Sinica, 2009, 48(1):109-122.
[32] 刘丽静, 杨芝林, 吴亚生.新疆塔里木盆地塔中地区上奥陶统良里塔格组钙化蓝细菌化石[J].古生物学报, 2011, 50(4):492-510. Liu Lijing, Yang Zhilin, Wu Yasheng.Calcified cyanobacteria from the Upper Ordovician Lianglitaga Formation, Central Tarim Basin, Xinjiang[J].Acta Palaeontologica Sinica, 2011, 50(4):492-510.
[33] 漆立新.塔里木盆地下古生界碳酸盐岩大油气田勘探实践与展望[J].石油与天然气地质, 2014.6(35):771-779. Qi Lixin.Exploration practice and prospects of giant carbonate field in the Lower Paleozoic of Tarim Basin.Oil & Gas Geology, 2014.6(35):771-779.
[34] 黄太柱, 蒋华山, 马庆佑.塔里木盆地下古生界碳酸盐岩油气成藏特征[J].石油与天然气地质, 2014.35(6):780-787. Huang Taizhu, Jiang Huashan, Ma Qingyou.Hydrocarbon accumulation characteristics in Lower Paleozoic Carbonate reservoirs of Tarim Basin[J].Oil & Gas Geology, 2014.35(6):780-787.
[35] 郑孟林, 王毅, 金之钧, 等.塔里木盆地叠合演化与油气聚集[J].石油与天然气地质, 2014.35(6):925-934. Zheng Menglin, Wang Yi, Jin Zhijun, et al.Superimposition, evolution and petroleum accumulation of Tarim Basin.Oil & Gas Geology, 2014.35(6):925-934.
[36] 宋立勋, 刘万祥.塔里木地台震旦纪古地理概貌[J].新疆石油地质, 1990, 11(3):199-203. Song L Y, Liu W X.Central apperance of Sinian Palaeogeoraphy of Tarim platform[J].XinJiang Petroleum Geology, 1990, 11(3):199-203.
[37] 张增耀, 杨松岭.塔里木盆地内震旦系特征[J].海相油气地质, 2007, 12(2):51-56. Zhang Zhenyao, Yang Songlin.Characteristics of Intrabasinal Sinian Sedimentary System in Tarim Basin[J].Marine oil & gas geology, 2007, 12(2):51-56.
[38] 叶德胜.塔里木盆地东北地区震旦-奥陶系白云岩的储集性[J].石油实验地质, 1992, 14(2):125-134. Ye Desheng.Reservoir property of the Sinian-Ordovician dolomites in the northeast Tarim basin[J].Petroleum Geology & Experimental, 1992, 14(2):125-134.
[39] 叶德胜.塔里木盆地北部震旦系至奥陶系白云岩的岩石学及地球化学特征[J].地球化学, 1993, 93(1):1-9. Ye Desheng.Lithology and geochemical characteristics of the Sinian-Ordovician dolomites in the northern Tarim basin[J].Geochimica, 1993, 93(1):1-9.
[40] 刘永福, 桑洪, 孙雄伟, 等.塔里木盆地东部震旦-寒武白云岩类型及成因[J].西南石油大学学报, 2008, 30(5):27-31. Liu Yongfu, Sang Hong, Sun Xiongwei et al.The types and genesis of Cambrian and Siinurian dolostone in Eastern Tarim Basin[J].Jounal of Southwest Petroleum University(Science & Technology Edition) , 2008, 30(5):27-31.
[41] 何金有.塔里木盆地震旦系古岩溶储层研究及油气勘探意义-何金有.北京:中国石油勘探开发研究院, 2010. He Jinyou.Study of the Sinian Karsted reservoirs of Tarim basin and its siginificane for petroleum exploration.Beijing:Reserch Institute of Petroleum Exploration and Development, Petrochina, 2010.
[42] 程裕淇, 王泽九, 黄枝高.中国地层典·总论[M].北京:地质出版社, 2009. Cheng Yuqi, Wang Zejiu, Huang Zhigao.General Treatise of Chinese strata[M].Beijing:Geological Press, 2009.
[43] 梁玉左, 朱士兴, 高振家, 等.叠层石研究的新进展-微生物岩[J].中国区域地质, 1995, (1):57-65. Liang Yuzuo, Zhu Shixing, Gao Zhenjia, et al.New progress in the study of stratomatilites-microbialite[M].Regional Geology of China, 1995, (1):57-65.
[44] 梁玉左, 朱士兴, 高振家, 等.叠层石研究的新进展-微生物岩[J].中国区域地质, 1995, (1):57-65. Liang Yuzuo, Zhu Shixing, Gao Zhenjia et al.New progress in the study of stromatomalites-microbialite[J].Regional Geology of China, 1995, (1):57-65.
[45] 王杰琼, 刘波, 罗平, 等.塔里木盆地西北缘震旦系混积岩类型及成因[J].成都理工大学学报(自然科学版).41(3):339-346. Wang Jieqiong, Liu Bo, Luo Ping et al.Classification and genesis of Sinian mixosedimentite from northwest margin of Tarim basin, China[J].Journal of Chengdu University of Technology(Science & Technology Editioin), 41(3):339-346.
[46] 梅冥相.微生物席的特征和属性:微生物席沉积学的理论基础[J].古地理学报, 2014, 16(3):285-304. Mei Mingxiang.Feature and nature of microbial-mat:Theoretical basis of microbial-mat sedimentology[J].Journal of Paleogeography, 2014, 16(3):285-304.
[47] Cohen Y.Photosynthesis in cyanobacterial mats and its relation to the sulfur cycle:A model for microbial sulfur interactions.In:Cohen Y, Rosenberg E( eds).Microbial Mats:Physiological Ecology of Benthic Microbial Communities[M].Washington:ASM, 1989:22-36.
[48] Wachendorfer V, Krumbein W E, Schellnhuber H J.Bacteriogenic porosity of marine sediments:A case of biomorphogenesis of sedimentary rocks.In:Krumbein W E, Paterson D M, Stal L J ( eds) .Biostabilization of Sediments[M].Oldenburg:Bibliotheks Informations system( BIS), 1994:203-220.
[49] 张荫本.震旦纪白云岩中的葡萄状构造成因初探[J].石油实验地质, 1980, 4:40-43. Zhang Yinben.Preliminary study on the botryoidal structures in the Sinian dolostones[J].Petroleum Geology & Experimental, 1980, 4:40-43.
[50] 向芳, 洪德, 张锦泉.资阳地区震旦系灯影组白云岩中葡萄花边的成因研究[J].矿物岩石, 1998, 18:136-138. Xiang Fang, Hong De, Zhang JjinQuan.Studying on the origin of botryo idal lace in dolomitite of Dengying Formation, Sinian from Ziyang Sichuan[J].Journal of Mineral Petrology, 1998, 18:136-138.
[51] 施泽进, 梁平, 王勇, 等.川东南地区灯影组葡萄石地球化学特征及成因分析[J].岩石学报, 2011, 27(8):2263-2271. Shi Zhejing, Liang Ping, Wang Yong, et al.Geochemical characteristics and genesis of grapestone in Sinian Dengying Formation in south-eastern Sichuan basin[J].Acta Petrologica Sinica, 2011, 27(8):2263-2271.
[52] 方少仙, 侯方浩, 董兆雄.上震旦统灯影组中非叠层石生态系兰细菌白云岩[J].沉积学报, 2003.21(1):96-105. Fang Shaoxian Hou Fanghao, Dong Zhaoxiong.Non-stomatolite Ecologic System cyanobacteria dolostone in Dengying Formation of Upper Sinian[J].Acta Sedmentologica Sinica, 2003, 21(1):96-105.