塔北地区上奥陶统良里塔格组台缘带分段性及石油地质意义
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摘要
碳酸盐岩台缘带类型对储层形成与油气产能具有重要的控制作用。利用塔北地区大量最新的地震资料与钻井资料,通过上奥陶统良里塔格组地层厚度变化刻画台缘带平面展布,基于台缘带地层坡度的计算揭示其不同段台缘类型的差异。在此基础上,探讨台缘带分段性对储层发育的控制作用。结果表明:①良里塔格组台缘带具有明显地层加厚的特点,平面上环塔北古隆起呈条带状展布,长约240km、宽约10～20km,面积达2600km~2。②基于台缘带地层坡度的变化,明确了良里塔格组台缘带沿东西方向表现为不同的类型,具有一定的分段性。西段为弱镶边型台地边缘,分布在英买力—哈拉哈塘—托普台地区,地震响应为向盆地方向减薄的楔形反射,地层坡度较大,介于1°～3°;东段为宽缓的缓坡型台地边缘,分布在塔河东部—轮古东—于奇地区,在地震剖面上由台地向盆地方向表现为一个波谷同相轴逐渐变细直至消失,地层坡度较小,介于0.2°～1°。③台缘带的分段性造成东、西段储层发育的差异性。西段储层品质好,厚度大,横向变化大;东段储层品质稍差,厚度小,平面分布广。塔北地区良里塔格组台缘带分段性对于优选有利勘探区带具有一定的指导意义。
Carbonate platform margin types play an important role in reservoir formation and oil and gas productivity.Based on newly acquired 3 Dseismic data and the latest drilling data,first we obtain the distribution of Lianglitage platform margins with platform margin strata thickness variations,and calculate different platform margin types with strata slopes in the study area.Then we analyze the control of margin types on reservoir development and oil and gas accumulation.The following understandings are obtained:(1)In Lianglitage platform margin,strata become obviously thicker,the Tabei palaeo-uplift is banded near EW surrounding with about 240 km long from east to west and 10～20 km wide from north to south,the total area is about 2600 km2;(2)Based on the stratigraphic slope variation in platform margin,the Lianglitag platform margin shows as different margin types along the east-west direction and has certain segments.The western part located in Yingmaili-HalahatangTuoputai area is weak rimmed carbonate platform margin with steep margin slope(1°to 3°).Seismic response of the platform margin is a cuneate reflection thinning to the basin.The eastern part located in eastern Tahe-Lungudong-Yuqi area is ramp type platform margin with gentle margin slope(0.2°to1°);On seismic sections,the platform margin is shown as a trough gradually tapering to disappear to the basin.(3)The segments of the Lianglitage platform margin resulted in the reservoir difference in these two parts.Reservoirs in the western part are thick and good quality,but with large lateral variation.Reservoirs in the eastern are part thin and poor quality,but with wide distribution.The segmentation of Lianglitage platform margin has important significance for selecting favorable exploration area in Tabei.
Carbonate platform margin types play an important role in reservoir formation and oil and gas productivity.Based on newly acquired 3 Dseismic data and the latest drilling data,first we obtain the distribution of Lianglitage platform margins with platform margin strata thickness variations,and calculate different platform margin types with strata slopes in the study area.Then we analyze the control of margin types on reservoir development and oil and gas accumulation.The following understandings are obtained:(1)In Lianglitage platform margin,strata become obviously thicker,the Tabei palaeo-uplift is banded near EW surrounding with about 240 km long from east to west and 10～20 km wide from north to south,the total area is about 2600 km2;(2)Based on the stratigraphic slope variation in platform margin,the Lianglitag platform margin shows as different margin types along the east-west direction and has certain segments.The western part located in Yingmaili-HalahatangTuoputai area is weak rimmed carbonate platform margin with steep margin slope(1°to 3°).Seismic response of the platform margin is a cuneate reflection thinning to the basin.The eastern part located in eastern Tahe-Lungudong-Yuqi area is ramp type platform margin with gentle margin slope(0.2°to1°);On seismic sections,the platform margin is shown as a trough gradually tapering to disappear to the basin.(3)The segments of the Lianglitage platform margin resulted in the reservoir difference in these two parts.Reservoirs in the western part are thick and good quality,but with large lateral variation.Reservoirs in the eastern are part thin and poor quality,but with wide distribution.The segmentation of Lianglitage platform margin has important significance for selecting favorable exploration area in Tabei.
引文
[1] Khalifa M A,Farouk S,Hassan A M.Carbonate platform facies development of the Turonian Wata Formation in central and eastern Sinai,Egypt[J].Journal of African Earth Sciences,2016,124(6):126-138.
[2] 邹才能,徐春春,汪泽成,等.四川盆地台缘带礁滩体大气区地质特征与形成条件[J].石油勘探与开发,2011,38(6):641-650.ZOU Caineng,XU Chunchun,WANG Zecheng,et al.Geological characteristics and forming conditions of the large platform margin reef-shoal gas province in the Sichuan Basin[J].Petroleum Exploration and Development,2011,38(6):641-650.
[3] 杨海军,邬光辉,韩剑发,等.塔里木盆地中央隆起带奥陶系碳酸盐岩台缘带油气富集特征[J].石油学报,2007,28(4):26-30.YANG Haijun,WU Guanghui,HAN Jianfa,et al.Characteristics of hydrocarbon enrichment along the Ordovician carbonate platform margin in the central uplift of Tarim Basin[J].Acta Petrolei Sinica,2007,28(4):26-30.
[4] 赵文智,沈安江,胡素云,等.中国碳酸盐岩储集层大型化发育的地质条件与分布特征[J].石油勘探与开发,2012,39(1):1-12.ZHAO Wenzhi,SHEN Anjiang,HU Suyun,et al.Geological conditions and distributional features of large-scale carbonate reservoirs onshore China[J].Petroleum Exploration and Development,2012,39(1):1-12.
[5] 乔博,高志前,樊太亮,等.塔里木盆地寒武系台缘结构特征及其演化[J].断块油气田,2014,21(1):7-11.QIAO Bo,GAO Zhiqian,FAN Tailiang,et al.Structural characteristics and evolution of Cambrian platform margin in Tarim Basin[J].Fault-Block Oil&Gas Field,2014,21(1):7-11.
[6] 倪新峰,沈安江,陈永权,等.塔里木盆地寒武系碳酸盐岩台地类型、台缘分段特征及勘探启示[J].天然气地球科学,2015,26(7):1245-1253.NI Xinfeng,SHEN Anjiang,CHEN Yongquan,et al.Cambrian carbonate platform types,platform margin segmentation characteristics and exploration enlightenment in Tarim Basin[J].Natural Gas Geoscience,2015,26(7):1245-1253.
[7] 孟祥杰,高志前,樊太亮,等.塔里木盆地中—下奥陶统台缘结构特征及油气指示意义[J].新疆石油地质,2015,36(3):293-298.MENG Xiangjie,GAO Zhiqian,FAN Tailiang,et al.Structural characteristics of carbonate platform margins in Lower-Middle Ordovician of Tarim Basin and related hydrocarbon implication[J].XinJiang Petroleum Geology,2015,36(3):293-298.
[8] 肖莹莹.塔里木盆地寒武—奥陶系台地结构特征及其对烃源岩的制约[D].北京:中国地质大学(北京),2011.
[9] Gao Z,Fan T.Carbonate platform-margin architecture and its influence on Cambrian-Ordovician reef-shoal development,Tarim Basin,NW China[J].Marine and Petroleum Geology,2015,68(12):291-306.
[10] 刘春晓,杨小波,钱利.新疆塔中地区奥陶系地层划分与岩性研究[J].地层学杂志,2009,33(2):217-224.LIU Chunxiao,YANG Xiaobo,QIAN Li.Stratigraphic division and lithostratigraphic characterization of the Ordovician system in the Tazhong Area of the Tarim Basin[J].Journal of Stratigraphy,2009,33(2):217-224.
[11] 陈轩,赵宗举,张宝民,等.塔里木盆地塔中孤立台地北缘上奥陶统良里塔格组精细沉积建模[J].沉积学报,2009,27(5):1002-1011.CHEN Xuan,ZHAO Zongju,ZHANG Baomin,et al.Delicate sedimentary model to Lianglitage Formation of Upper Ordovician in the Northern margin of isolated platform in the center of Tarim Basin[J].Acta Sedimentologica Sinica,2009,27(5):1002-1011.
[12] 何碧竹,焦存礼,王生朗,等.塔里木盆地塔中地区上奥陶统近环带状台地边缘相带特征及勘探前景[J].地质学报,2009,83(7):1039-1046.HE Bizhu,JIAO Cunli,WANG Shenglang,et al.Characteristics and exploration prospect of carbonate platform margin of Late Ordovician Lianglitage Formation in the Tazhong Area,Tarim Basin[J].Acta Geologica Sinica,2009,83(7):1039-1046.
[13] 孙玉善,韩杰,张丽娟,等.塔里木盆地塔中地区上奥陶统礁滩体基质次生孔隙成因——以塔中62井区为例[J].石油勘探与开发,2007,34(5):541-547.SUN Yushan,HAN Jie,ZHANG Lijuan,et al.Genesis of reef flat body matrix secondary pores in Upper Ordovician in central area of Tarim Basin:A case from Well 62 field of Central Tarim[J].Petroleum Exploration and Development,2007,34(5):541-547.
[14] 高志前,樊太亮,刘典波,等.塔里木盆地塔中南坡台缘带油气成藏条件[J].石油勘探与开发,2008,35(4):437-443.GAO Zhiqian,FAN Tailiang,LIU Dianbo,et al.Re-servoir-forming conditions of platform margin belt in southern slope of Tazhong,Tarim Basin[J].Petroleum Exploration and Development,2008,35(4):437-443.
[15] 刘嘉庆,李忠,韩银学,等.塔河油田上奥陶统良里塔格组碳酸盐岩沉积地球化学特征与台地演化[J].地质科学,2010,45(1):278-291.LIU Jiaqing,LI Zhong,HAN Yinxue,et al.Characte-ristics of sedimentary geochemistry and evolution of platform of the Lianglitag Formation carbonate,Upper Ordovician in Tahe Oilfield[J].Chinese Journal of Geology,2010,45(1):278-291.
[16] 刘嘉庆,李忠,黄君凑,等.塔里木盆地良里塔格组沉积环境差异及其对碳酸盐储层发育的制约[J].中国科学:地球科学,2012,45(12):1802-1816.LIU Jiaqing,LI Zhong,HUANG Juncou,et al.Distinct sedimentary environments and their influence on carbonate reservoir evolution of the Lianglitag Formation in the Tarim Basin,Northwest China[J].Science China:Earth Sciences,2012,45(12):1802-1816.
[17] 候明才,万梨,傅恒,等.塔河南盐下地区上奥陶统良里塔格组沉积环境分析[J].成都理工大学学报(自然科学版),2006,33(5):509-517.HOU Mingcai,WAN Li,FU Heng,et al.Study on the sedimentary environment of the Upper Ordovician Lianglitage Formation in the south of Tarim River,China[J].Journal of Chengdu University of Techno-logy(Science & Technology Edition),2006,33(5):509-517.
[18] 马青,赵学钦,陈沛,等.轮南周缘地区奥陶系碳酸盐岩沉积相发育规律[J].西南石油大学学报,2007,29(4):26-30.MA Qing,ZHAO Xueqin,CHEN Pei,et al.The law of sedimentary facies development of Ordovician carbonate rocks in the Lunnan’s periphery,Tarim Basin[J].Journal of Southwest Petroleum University,2007,29(4):26-30.
[19] 赵学钦,杨海军,马青,等.塔北奥陶系碳酸盐岩沉积演化特征及台地发育模式[J].沉积与特提斯地质,2014,34(2):36-43.ZHAO Xueqin,YANG Haijun,MA Qing,et al.Sedimentary evolution and platform development models for the Ordovician carbonate rocks in northern Tarim Basin[J].Sedimentary Geology and Tethyan Geology,2014,34(2):36-43.
[20] 韩杰,袁源,吴梅莲,等.新疆塔里木盆地轮古东气田良里塔格组沉积特征及其与油气关系[J].矿物岩石地球化学通报,2016,35(4):710-719.HAN Jie,YUAN Yuan,WU Meilian,et al.The sedimentation characteristics and the relationship with the hydrocarbon of the Lianglitage Formation in the Lungudong Gas Field,Tarim Basin,Xinjiang,China[J].Bulletin of Mineralogy,Petrology and Geochemistry,2016,35(4):710-719.
[21] 毛雪莲,马青,刘伟,等.哈拉哈塘地区良里塔格组沉积特征分析[J].岩性油气藏,2012,24(3):21-27.MAO Xuelian,MA Qing,LIU Wei,et al.Sedimentary characteristics of the Upper Ordovician Lianglitage Formation in Halahatang area[J].Lithologic Reservoirs,2012,24(3):21-27.
[22] 安海亭,李海银,王建忠,等.塔北地区构造和演化特征及其对油气成藏的控制[J].大地构造与成矿学,2009,33(1):142-147.AN Haiting,LI Haiyin,WANG Jianzhong,et al.Tectonic evolution and its controlling on oil and gas accumulation in the Northern Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):142-147.
[23] 马德波,陈利新,陶小晚,等.塔里木盆地哈拉哈塘地区构造演化及其油气地质意义[J].地质科学,2018,53(1):87-104.MA Debo,CHEN Lixin,TAO Xiaowan,et al.The tectonic evolution and its petroleum geological significance in Halahatang area,Tarim Basin[J].Chinese Journal of Geology,2018,53(1):87-104.
[24] James L W.Characteristics of carbonate-platform margins[J].AAPG Bulletin,1974,58(5):810-824.
[25] 曾清波,张功成,廖宗宝,等.珠江口盆地东沙隆起早中新世台缘带特征及勘探方向[J].海相油气地质,2015,20(1):17-25.ZENG Qingbo,ZHANG Gongcheng,LIAO Zongbao,et al.Geological features and prospecting potential of Early Miocence platform margin belt in Dongsha Uplift,Zhujiangkou Basin[J].Marine Origin Petroleum Geology,2015,20(1):17-25.
[26] Matteo D L,Jhosnella S,Gianluca F,et al.Facies and seismic analysis of the Late Carboniferous-Early Permian Finnmark carbonate platform(southern Norwegian Barents Sea):An assessment of the carbonate factories and depositional geometries[J].Marine and Petroleum Geology,2017,79(3):372-393.
[27] 吴晓川,蒲仁海,张功成,等.琼东南盆地南部深水区碳酸盐岩台地的地震解释[J].石油地球物理勘探,2017,52(2):381-391.WU Xiaochuan,PU Renhai,ZHANG Gongcheng,et al.Seismic interpretation of carbonate platform in the southern deepwater area,Qiongdongnan Basin[J].Oil Geophysical Prospecting,2017,52(2):381-391.
[28] Hartwig V H,Hermann B,Charlotte M K,et al.3-D seismic analysis of a carbonate platform in the Molasse Basin: reef distribution and internal separation with seismic attributes[J].Tectonophysics,2012,572-573(20):16-25.
[29] 刘忠亮,张成富,张渊,等.Oriente盆地L-I-Y油田Hollin组与Napo组沉积微相研究[J].石油物探,2017,56(4):581-588.LIU Zhongliang,ZHANG Chengfu,ZHANG Yuan,et al.Sedimentary microfacies of the Hollin and Napo formation in the L-I-Y Oilfield,Oriente Basin[J].Geophysical Prospecting for Petroleum,2017,56(4):581-588.
[30] Cathro L,Austin Jr,Graham D M.Progradation along a deeply submerged Oligocene-Miocene heterozoan carbonate shelf: How sensitive are clinoforms to sea level variations?[J].AAPG Bulletin,2003,87(10):1547-1574.
[31] 金振奎,石良,高白水,等.碳酸盐岩沉积相及相模式[J].沉积学报,2013,31(6):965-979.JIN Zhenkui,SHI Liang,GAO Baishui,et al.Carbo-nate facies and facies models[J].Acta Sedimentologica Sinica,2013,31(6):965-979.
[32] 赵宗举,周新源,王招明,等.塔里木盆地奥陶系边缘相分布及储层主控因素[J].石油与天然气地质,2007,28(6):738-745.ZHAO Zongju,ZHOU Xinyuan,WANG Zhaoming,et al.Distribution of marginal facies and main controlling factors of reservoirs in the Ordovician,the Tarim Basin[J].Oil & Gas Geology,2007,28(6):738-745.
[33] 赵文智,沈安江,周进高,等.礁滩储集层类型、特征、成因及勘探意义——以塔里木和四川盆地为例[J].石油勘探与开发,2014,41(3):257-268.ZHAO Wenzhi,SHEN Anjiang,ZHOU Jingao,et al.Types,characteristics,origin and exploration significance of reef-shoal reservoirs:A case study of Tarim Basin,NW China and Sichuan Basin,SW China[J].Petroleum Exploration and Development,2014,41(3):257-268.
[34] 顾家裕,张兴阳,罗平,等.塔里木盆地奥陶系台地边缘生物礁、滩发育特征[J].石油与天然气地质,2005,26(3):277-284.GU Jiayu,ZHANG Xingyang,LUO Ping,et al.Development characteristics of organic reef-bank complex on Ordovician carbonate platform margin in Ta-rim Basin[J].Oil & Gas Geology,2005,26(3):277-284.
[35] 赵明胜.塔里木盆地奥陶系不同台地边缘礁滩体类型、迁移及储集体差异性研究[D].四川成都:成都理工大学,2014.ZHAO Mingsheng.The Research of Differences on Types,Migration and Reservoir of Reef Flat Body in Platform Edge during the Ordovician in Tarim Basin[D].Chengdu University of Technology,Chengdu,Sichuan,2014.
[36] 马永生.碳酸盐岩微相——分析、解释及应用[M].北京:地质出版社,2006.
[37] 朱超,刘占国,杨少勇,等.利用相控分频反演预测英西湖相碳酸盐岩储层[J].石油地球物理勘探,2018,53(4):832-841.ZHU Chao,LIU Zhanguo,YANG Shaoyong,et al.Lacustrine carbonate reservoir prediction in Yingxi,Qaidam Basin with facies-constrained and segmented-frequency-band inversion[J].Oil Geophysical Prospecting,2018,53(4):832-841.
[38] 喻林,何燕,陈红,等.基于古地貌恢复的湖湘碳酸盐岩沉积模式研究[J].石油地球物理勘探,2016,51(增刊1):126-130.YU Lin,HE Yan,CHEN Hong,et al.Analysis of lacustrine carbonate sedimentary patterns based on paleo-geomorphic restoration[J].Oil Geophysical Prospecting,2016,51(S1):126-130.
[39] 马灵伟,顾汉明,赵迎月,等.应用随机介质正演模拟刻画深水区台缘礁碳酸盐岩储层[J].石油地球物理勘探,2013,48(4):583-591.MA Lingwei,GU Hanming,ZHAO Yingyue,et al.Sculpturing platform-edge reef carbonate reservoirs in deep-water with random media forward modelling[J].Oil Geophysical Prospecting,2013,48(4):583-591.
[40] 罗平,张兴阳,顾家裕,等.塔里木盆地奥陶系生物礁露头的地球物理特征[J].沉积学报,2003,21(3):423-428.LUO Ping,ZHANG Xingyang,GU Jiayu,et al.Geophysical characteristics of Ordovician reef outcrops in Tarim Basin[J].Acta Sedimentologica Sinica,2003,21(3):423-428.
[41] 赵文智,沈安江,胡素云,等.中国碳酸盐岩储集层大型化发育的地质条件与分布特征[J].石油勘探与开发,2012,39(1):1-12.ZHAO Wenzhi,SHEN Anjiang,HU Suyun,et al.Geological conditions and distributional features of large-scale carbonate reservoirs onshore China[J].Petroleum Exploration and Development,2012,39(1):1-12.
[2] 邹才能,徐春春,汪泽成,等.四川盆地台缘带礁滩体大气区地质特征与形成条件[J].石油勘探与开发,2011,38(6):641-650.ZOU Caineng,XU Chunchun,WANG Zecheng,et al.Geological characteristics and forming conditions of the large platform margin reef-shoal gas province in the Sichuan Basin[J].Petroleum Exploration and Development,2011,38(6):641-650.
[3] 杨海军,邬光辉,韩剑发,等.塔里木盆地中央隆起带奥陶系碳酸盐岩台缘带油气富集特征[J].石油学报,2007,28(4):26-30.YANG Haijun,WU Guanghui,HAN Jianfa,et al.Characteristics of hydrocarbon enrichment along the Ordovician carbonate platform margin in the central uplift of Tarim Basin[J].Acta Petrolei Sinica,2007,28(4):26-30.
[4] 赵文智,沈安江,胡素云,等.中国碳酸盐岩储集层大型化发育的地质条件与分布特征[J].石油勘探与开发,2012,39(1):1-12.ZHAO Wenzhi,SHEN Anjiang,HU Suyun,et al.Geological conditions and distributional features of large-scale carbonate reservoirs onshore China[J].Petroleum Exploration and Development,2012,39(1):1-12.
[5] 乔博,高志前,樊太亮,等.塔里木盆地寒武系台缘结构特征及其演化[J].断块油气田,2014,21(1):7-11.QIAO Bo,GAO Zhiqian,FAN Tailiang,et al.Structural characteristics and evolution of Cambrian platform margin in Tarim Basin[J].Fault-Block Oil&Gas Field,2014,21(1):7-11.
[6] 倪新峰,沈安江,陈永权,等.塔里木盆地寒武系碳酸盐岩台地类型、台缘分段特征及勘探启示[J].天然气地球科学,2015,26(7):1245-1253.NI Xinfeng,SHEN Anjiang,CHEN Yongquan,et al.Cambrian carbonate platform types,platform margin segmentation characteristics and exploration enlightenment in Tarim Basin[J].Natural Gas Geoscience,2015,26(7):1245-1253.
[7] 孟祥杰,高志前,樊太亮,等.塔里木盆地中—下奥陶统台缘结构特征及油气指示意义[J].新疆石油地质,2015,36(3):293-298.MENG Xiangjie,GAO Zhiqian,FAN Tailiang,et al.Structural characteristics of carbonate platform margins in Lower-Middle Ordovician of Tarim Basin and related hydrocarbon implication[J].XinJiang Petroleum Geology,2015,36(3):293-298.
[8] 肖莹莹.塔里木盆地寒武—奥陶系台地结构特征及其对烃源岩的制约[D].北京:中国地质大学(北京),2011.
[9] Gao Z,Fan T.Carbonate platform-margin architecture and its influence on Cambrian-Ordovician reef-shoal development,Tarim Basin,NW China[J].Marine and Petroleum Geology,2015,68(12):291-306.
[10] 刘春晓,杨小波,钱利.新疆塔中地区奥陶系地层划分与岩性研究[J].地层学杂志,2009,33(2):217-224.LIU Chunxiao,YANG Xiaobo,QIAN Li.Stratigraphic division and lithostratigraphic characterization of the Ordovician system in the Tazhong Area of the Tarim Basin[J].Journal of Stratigraphy,2009,33(2):217-224.
[11] 陈轩,赵宗举,张宝民,等.塔里木盆地塔中孤立台地北缘上奥陶统良里塔格组精细沉积建模[J].沉积学报,2009,27(5):1002-1011.CHEN Xuan,ZHAO Zongju,ZHANG Baomin,et al.Delicate sedimentary model to Lianglitage Formation of Upper Ordovician in the Northern margin of isolated platform in the center of Tarim Basin[J].Acta Sedimentologica Sinica,2009,27(5):1002-1011.
[12] 何碧竹,焦存礼,王生朗,等.塔里木盆地塔中地区上奥陶统近环带状台地边缘相带特征及勘探前景[J].地质学报,2009,83(7):1039-1046.HE Bizhu,JIAO Cunli,WANG Shenglang,et al.Characteristics and exploration prospect of carbonate platform margin of Late Ordovician Lianglitage Formation in the Tazhong Area,Tarim Basin[J].Acta Geologica Sinica,2009,83(7):1039-1046.
[13] 孙玉善,韩杰,张丽娟,等.塔里木盆地塔中地区上奥陶统礁滩体基质次生孔隙成因——以塔中62井区为例[J].石油勘探与开发,2007,34(5):541-547.SUN Yushan,HAN Jie,ZHANG Lijuan,et al.Genesis of reef flat body matrix secondary pores in Upper Ordovician in central area of Tarim Basin:A case from Well 62 field of Central Tarim[J].Petroleum Exploration and Development,2007,34(5):541-547.
[14] 高志前,樊太亮,刘典波,等.塔里木盆地塔中南坡台缘带油气成藏条件[J].石油勘探与开发,2008,35(4):437-443.GAO Zhiqian,FAN Tailiang,LIU Dianbo,et al.Re-servoir-forming conditions of platform margin belt in southern slope of Tazhong,Tarim Basin[J].Petroleum Exploration and Development,2008,35(4):437-443.
[15] 刘嘉庆,李忠,韩银学,等.塔河油田上奥陶统良里塔格组碳酸盐岩沉积地球化学特征与台地演化[J].地质科学,2010,45(1):278-291.LIU Jiaqing,LI Zhong,HAN Yinxue,et al.Characte-ristics of sedimentary geochemistry and evolution of platform of the Lianglitag Formation carbonate,Upper Ordovician in Tahe Oilfield[J].Chinese Journal of Geology,2010,45(1):278-291.
[16] 刘嘉庆,李忠,黄君凑,等.塔里木盆地良里塔格组沉积环境差异及其对碳酸盐储层发育的制约[J].中国科学:地球科学,2012,45(12):1802-1816.LIU Jiaqing,LI Zhong,HUANG Juncou,et al.Distinct sedimentary environments and their influence on carbonate reservoir evolution of the Lianglitag Formation in the Tarim Basin,Northwest China[J].Science China:Earth Sciences,2012,45(12):1802-1816.
[17] 候明才,万梨,傅恒,等.塔河南盐下地区上奥陶统良里塔格组沉积环境分析[J].成都理工大学学报(自然科学版),2006,33(5):509-517.HOU Mingcai,WAN Li,FU Heng,et al.Study on the sedimentary environment of the Upper Ordovician Lianglitage Formation in the south of Tarim River,China[J].Journal of Chengdu University of Techno-logy(Science & Technology Edition),2006,33(5):509-517.
[18] 马青,赵学钦,陈沛,等.轮南周缘地区奥陶系碳酸盐岩沉积相发育规律[J].西南石油大学学报,2007,29(4):26-30.MA Qing,ZHAO Xueqin,CHEN Pei,et al.The law of sedimentary facies development of Ordovician carbonate rocks in the Lunnan’s periphery,Tarim Basin[J].Journal of Southwest Petroleum University,2007,29(4):26-30.
[19] 赵学钦,杨海军,马青,等.塔北奥陶系碳酸盐岩沉积演化特征及台地发育模式[J].沉积与特提斯地质,2014,34(2):36-43.ZHAO Xueqin,YANG Haijun,MA Qing,et al.Sedimentary evolution and platform development models for the Ordovician carbonate rocks in northern Tarim Basin[J].Sedimentary Geology and Tethyan Geology,2014,34(2):36-43.
[20] 韩杰,袁源,吴梅莲,等.新疆塔里木盆地轮古东气田良里塔格组沉积特征及其与油气关系[J].矿物岩石地球化学通报,2016,35(4):710-719.HAN Jie,YUAN Yuan,WU Meilian,et al.The sedimentation characteristics and the relationship with the hydrocarbon of the Lianglitage Formation in the Lungudong Gas Field,Tarim Basin,Xinjiang,China[J].Bulletin of Mineralogy,Petrology and Geochemistry,2016,35(4):710-719.
[21] 毛雪莲,马青,刘伟,等.哈拉哈塘地区良里塔格组沉积特征分析[J].岩性油气藏,2012,24(3):21-27.MAO Xuelian,MA Qing,LIU Wei,et al.Sedimentary characteristics of the Upper Ordovician Lianglitage Formation in Halahatang area[J].Lithologic Reservoirs,2012,24(3):21-27.
[22] 安海亭,李海银,王建忠,等.塔北地区构造和演化特征及其对油气成藏的控制[J].大地构造与成矿学,2009,33(1):142-147.AN Haiting,LI Haiyin,WANG Jianzhong,et al.Tectonic evolution and its controlling on oil and gas accumulation in the Northern Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):142-147.
[23] 马德波,陈利新,陶小晚,等.塔里木盆地哈拉哈塘地区构造演化及其油气地质意义[J].地质科学,2018,53(1):87-104.MA Debo,CHEN Lixin,TAO Xiaowan,et al.The tectonic evolution and its petroleum geological significance in Halahatang area,Tarim Basin[J].Chinese Journal of Geology,2018,53(1):87-104.
[24] James L W.Characteristics of carbonate-platform margins[J].AAPG Bulletin,1974,58(5):810-824.
[25] 曾清波,张功成,廖宗宝,等.珠江口盆地东沙隆起早中新世台缘带特征及勘探方向[J].海相油气地质,2015,20(1):17-25.ZENG Qingbo,ZHANG Gongcheng,LIAO Zongbao,et al.Geological features and prospecting potential of Early Miocence platform margin belt in Dongsha Uplift,Zhujiangkou Basin[J].Marine Origin Petroleum Geology,2015,20(1):17-25.
[26] Matteo D L,Jhosnella S,Gianluca F,et al.Facies and seismic analysis of the Late Carboniferous-Early Permian Finnmark carbonate platform(southern Norwegian Barents Sea):An assessment of the carbonate factories and depositional geometries[J].Marine and Petroleum Geology,2017,79(3):372-393.
[27] 吴晓川,蒲仁海,张功成,等.琼东南盆地南部深水区碳酸盐岩台地的地震解释[J].石油地球物理勘探,2017,52(2):381-391.WU Xiaochuan,PU Renhai,ZHANG Gongcheng,et al.Seismic interpretation of carbonate platform in the southern deepwater area,Qiongdongnan Basin[J].Oil Geophysical Prospecting,2017,52(2):381-391.
[28] Hartwig V H,Hermann B,Charlotte M K,et al.3-D seismic analysis of a carbonate platform in the Molasse Basin: reef distribution and internal separation with seismic attributes[J].Tectonophysics,2012,572-573(20):16-25.
[29] 刘忠亮,张成富,张渊,等.Oriente盆地L-I-Y油田Hollin组与Napo组沉积微相研究[J].石油物探,2017,56(4):581-588.LIU Zhongliang,ZHANG Chengfu,ZHANG Yuan,et al.Sedimentary microfacies of the Hollin and Napo formation in the L-I-Y Oilfield,Oriente Basin[J].Geophysical Prospecting for Petroleum,2017,56(4):581-588.
[30] Cathro L,Austin Jr,Graham D M.Progradation along a deeply submerged Oligocene-Miocene heterozoan carbonate shelf: How sensitive are clinoforms to sea level variations?[J].AAPG Bulletin,2003,87(10):1547-1574.
[31] 金振奎,石良,高白水,等.碳酸盐岩沉积相及相模式[J].沉积学报,2013,31(6):965-979.JIN Zhenkui,SHI Liang,GAO Baishui,et al.Carbo-nate facies and facies models[J].Acta Sedimentologica Sinica,2013,31(6):965-979.
[32] 赵宗举,周新源,王招明,等.塔里木盆地奥陶系边缘相分布及储层主控因素[J].石油与天然气地质,2007,28(6):738-745.ZHAO Zongju,ZHOU Xinyuan,WANG Zhaoming,et al.Distribution of marginal facies and main controlling factors of reservoirs in the Ordovician,the Tarim Basin[J].Oil & Gas Geology,2007,28(6):738-745.
[33] 赵文智,沈安江,周进高,等.礁滩储集层类型、特征、成因及勘探意义——以塔里木和四川盆地为例[J].石油勘探与开发,2014,41(3):257-268.ZHAO Wenzhi,SHEN Anjiang,ZHOU Jingao,et al.Types,characteristics,origin and exploration significance of reef-shoal reservoirs:A case study of Tarim Basin,NW China and Sichuan Basin,SW China[J].Petroleum Exploration and Development,2014,41(3):257-268.
[34] 顾家裕,张兴阳,罗平,等.塔里木盆地奥陶系台地边缘生物礁、滩发育特征[J].石油与天然气地质,2005,26(3):277-284.GU Jiayu,ZHANG Xingyang,LUO Ping,et al.Development characteristics of organic reef-bank complex on Ordovician carbonate platform margin in Ta-rim Basin[J].Oil & Gas Geology,2005,26(3):277-284.
[35] 赵明胜.塔里木盆地奥陶系不同台地边缘礁滩体类型、迁移及储集体差异性研究[D].四川成都:成都理工大学,2014.ZHAO Mingsheng.The Research of Differences on Types,Migration and Reservoir of Reef Flat Body in Platform Edge during the Ordovician in Tarim Basin[D].Chengdu University of Technology,Chengdu,Sichuan,2014.
[36] 马永生.碳酸盐岩微相——分析、解释及应用[M].北京:地质出版社,2006.
[37] 朱超,刘占国,杨少勇,等.利用相控分频反演预测英西湖相碳酸盐岩储层[J].石油地球物理勘探,2018,53(4):832-841.ZHU Chao,LIU Zhanguo,YANG Shaoyong,et al.Lacustrine carbonate reservoir prediction in Yingxi,Qaidam Basin with facies-constrained and segmented-frequency-band inversion[J].Oil Geophysical Prospecting,2018,53(4):832-841.
[38] 喻林,何燕,陈红,等.基于古地貌恢复的湖湘碳酸盐岩沉积模式研究[J].石油地球物理勘探,2016,51(增刊1):126-130.YU Lin,HE Yan,CHEN Hong,et al.Analysis of lacustrine carbonate sedimentary patterns based on paleo-geomorphic restoration[J].Oil Geophysical Prospecting,2016,51(S1):126-130.
[39] 马灵伟,顾汉明,赵迎月,等.应用随机介质正演模拟刻画深水区台缘礁碳酸盐岩储层[J].石油地球物理勘探,2013,48(4):583-591.MA Lingwei,GU Hanming,ZHAO Yingyue,et al.Sculpturing platform-edge reef carbonate reservoirs in deep-water with random media forward modelling[J].Oil Geophysical Prospecting,2013,48(4):583-591.
[40] 罗平,张兴阳,顾家裕,等.塔里木盆地奥陶系生物礁露头的地球物理特征[J].沉积学报,2003,21(3):423-428.LUO Ping,ZHANG Xingyang,GU Jiayu,et al.Geophysical characteristics of Ordovician reef outcrops in Tarim Basin[J].Acta Sedimentologica Sinica,2003,21(3):423-428.
[41] 赵文智,沈安江,胡素云,等.中国碳酸盐岩储集层大型化发育的地质条件与分布特征[J].石油勘探与开发,2012,39(1):1-12.ZHAO Wenzhi,SHEN Anjiang,HU Suyun,et al.Geological conditions and distributional features of large-scale carbonate reservoirs onshore China[J].Petroleum Exploration and Development,2012,39(1):1-12.