塔里木盆地奥陶系碳酸盐岩热液蚀变的地质与地球化学特征研究
|
摘要
本文研究塔中地区不同类型热液活动所引起的岩溶现象与蚀变现象,及其与储层发育的关系,从中提炼主导性的控制因素,将零散的野外地质现象和经验性总结提升为描述预测储层发育及其空间分布的规律,将为解决塔里木盆地的储层成因类型及成因机理、储层预测提供依据,也将为认识塔中碳酸盐岩油气藏的空间分布规律提供新视野。
本文综合采用矿物岩石学、地球化学和同位素示踪技术等手段,以及采用微量元素证据,重点探讨热液白云岩以及与热液白云岩相伴生的热液淋滤灰岩的野外地质特征,并总结归纳奥陶系碳酸盐岩经热液蚀变、淋滤后产物的矿物岩石学和地球化学特征并讨论热液流体的来源与性质,根据热液矿物共生关系、热液活动期次角度,识别了四类矿物组合。
观察并总结了存在的热液现象井位的岩芯和薄片资料,并根据对野外剖面热液蚀变的认识和理解,结合ZG8至ZG15区块的勘探实际,对塔里木热液相关储层的控制因素和储层进行了预测,提出了碳酸盐岩热液溶蚀储层预测模型,指出了有利于热液溶蚀型储层发育的因素以及热液岩溶储层的产出层位。
This paper abstracted controlling factors by reasch on karst and alteration caused by different types of hydrothermal activities and the connections with reservoir, Summarize the reserior formation prediction and spatial distribution regularities by bits and pieces of geologic phenomenon and the summing-up of experience. Aim to provide evidence of genetic type and the genesis of reservoir and reserior formation prediction and to lend a fresh perspective to realize the spatial distribution regularities of Carbonate in Ordovician in the center of Tarim Basin.
Based on Petrologic and geochemical methods、isotope tracing techniques and trace element, discuss the field geological phenomena of hydrothermal dolomite and hydrothermal leaching limestone associated with hydrothermal dolomite, summarize mineral petrologic and geochemical characteristics of hydrothermal product or leacheate in the Ordovician carbonate rocks, discuss the origin and nature of hydrothermal fluids, Identified four types of mineral assemblages from the view of hydrothermal mineral symbiotic relationship and hydrothermal active stages.
Observing and analyzing thin sections and cores of wells having hydrothermal alteration, based on awareness and understanding of hydrothermal alteration in the fild section, combined with the actual exploration of ZG8 to ZG15 block, predict reservoir and controlling factors of hydrothermal carbonate Reservoirs in Tarim Basin, propose a model of hydrothermal carbonate reservoirs, Pointed out the favorable facts of hydrothermal-realated reservoirs development and the horizon of hydrothermal Karst carbonate reservoir.
本文综合采用矿物岩石学、地球化学和同位素示踪技术等手段,以及采用微量元素证据,重点探讨热液白云岩以及与热液白云岩相伴生的热液淋滤灰岩的野外地质特征,并总结归纳奥陶系碳酸盐岩经热液蚀变、淋滤后产物的矿物岩石学和地球化学特征并讨论热液流体的来源与性质,根据热液矿物共生关系、热液活动期次角度,识别了四类矿物组合。
观察并总结了存在的热液现象井位的岩芯和薄片资料,并根据对野外剖面热液蚀变的认识和理解,结合ZG8至ZG15区块的勘探实际,对塔里木热液相关储层的控制因素和储层进行了预测,提出了碳酸盐岩热液溶蚀储层预测模型,指出了有利于热液溶蚀型储层发育的因素以及热液岩溶储层的产出层位。
This paper abstracted controlling factors by reasch on karst and alteration caused by different types of hydrothermal activities and the connections with reservoir, Summarize the reserior formation prediction and spatial distribution regularities by bits and pieces of geologic phenomenon and the summing-up of experience. Aim to provide evidence of genetic type and the genesis of reservoir and reserior formation prediction and to lend a fresh perspective to realize the spatial distribution regularities of Carbonate in Ordovician in the center of Tarim Basin.
Based on Petrologic and geochemical methods、isotope tracing techniques and trace element, discuss the field geological phenomena of hydrothermal dolomite and hydrothermal leaching limestone associated with hydrothermal dolomite, summarize mineral petrologic and geochemical characteristics of hydrothermal product or leacheate in the Ordovician carbonate rocks, discuss the origin and nature of hydrothermal fluids, Identified four types of mineral assemblages from the view of hydrothermal mineral symbiotic relationship and hydrothermal active stages.
Observing and analyzing thin sections and cores of wells having hydrothermal alteration, based on awareness and understanding of hydrothermal alteration in the fild section, combined with the actual exploration of ZG8 to ZG15 block, predict reservoir and controlling factors of hydrothermal carbonate Reservoirs in Tarim Basin, propose a model of hydrothermal carbonate reservoirs, Pointed out the favorable facts of hydrothermal-realated reservoirs development and the horizon of hydrothermal Karst carbonate reservoir.
引文
苌衡,张新艳,彭鑫岭,塔里木盆地塔中地区火成岩对油气勘探的影响[J].断块油气田,003,10(1)：5-8
陈汉林,贾成造,1997.塔里木盆地地质热事件研究[J].科学通报42(10)：1096-1099
邓胜徽,黄智斌,景秀春,等.塔里木盆地西部奥陶系内部不整合[J].地质论评54(6)：741-747
何莹,鲍志东,沈安江,等.塔里木盆地牙哈—英买力地区寒武系—下奥陶统白云岩形成机理[J].沉积学报,2006,24(6)：806-818.
胡受奚,叶瑛等.交代蚀变岩岩石学及找矿意义[M].北京：地质出版社,2004：3.
贾承造,魏国齐,姚惠君等,盆地构造演化与区域构造地质[M].北京：石油工业出版社1995：12
贾承造.中国塔里木盆地构造特征与油气[M].北京：石油工业出版社,1997：23
贾存善,马旭杰,饶丹,等.2007.塔河油田奥陶系油田水同位素特征及地质意义[J],石油实验地质,29(3)：292-297.
金之钧,张刘平,胡文瑄等,2002.沉积盆地深部流体的地球化学特征及油气成藏效应初探[J].地球科学-中国地质大学学报,27(6)：659-665
钱一雄,邹远荣,陈跃,等.塔里木盆地塔中西北部多期、多成因岩溶作用地质-地球化学表征—以中1井为例[J].沉积学报,2005,23(4)：596-603.
邵龙义,Jones T P.桂中晚二叠世碳酸盐岩碳同位素的地层学意义[J].沉积学报,1999,17(1)：84-88.
王安甲,初广震,黄文辉,等.2008.塔里木盆地奥陶系碳酸盐岩碳氧稳定同位素地球化学特征[J].成都理工大学学报(自然科学版),35(6)：700-704.
徐维胜,热液改造碳酸盐岩储层综合研究[J].内蒙古石油化工.2009,(1)：20-22.
张景廉,金之钧,等.2001.塔里木盆地深部地质流体与油气藏的关系.新疆石油地质,22(5)：371-375
张兴阳,张水昌,罗平,等.塔中地区晚燕山—喜马拉雅期油气调整与热液活动的关系[J].科学通报,2007,52(增1)：192-198.
张学丰,胡文,张军涛.白云岩成因相关问题及主要形成模式[J].地质科技情报,2006,25(5)：32-40.
周志毅.塔里木盆地各纪地层[M].北京：科学出版社,2001,35-102
朱金富,于炳松,黄文辉,等.塔里木盆地塔中地区晚寒武世—奥陶世碳酸盐岩碳、氧同位素特征[J].大庆石油地质与开发,2008,27(1)：40-42.
Adam J E, Rhodes M L. Dolomitization by seepage reflux[J]. AAPG Bulletin,1960, 44(12):1912-1920.
Badiozamani K. The dorag dolomitization model, application to the middle Ordovician of Wisconsin[J]. Journal of Sedimentary Research,1973,43(4): 965-984.
Boreen, T., and G. R. Davies,2004, Hydrothermal dolomite and leached limestones in a TCF gas play: The Ladyfern Slave Point reservoir, NEBC, in R. McAuley, ed., Dolomites-The spectrum: Mechanisms, models, reservoir development: Canadian Society of Petroleum Geologists, Seminar and Core Conference, January 13-15,2004, Calgary, Extended Abstracts, CD format.
Boreen, T., and K. Colquhoun,2001, Ladyfern, NEBC:Major gas discovery in the Devonian Slave Point Formation (abs.):Canadian Society of Petroleum Geologists, Annual Convention, Abstracts, p.112/1-5.
Bruckschen, P., S. Oesmann, and J. Veizer,1999, Isotope stratigraphy of the European Carboniferous:Proxy signals for ocean chemistry, climate and tectonics [J]. Chemical Geology, v.161,127-163.
Chow, N., Morad, S., Al-Asam, I.S.,1996. Origin of authigenic carbonates in Eocene to Quaternary sediments from the Artic Ocean and Norwegian-Greenland Sea[J]. Proc. Ocean Drilling Program Sci. Res., vol.151, pp.415-434.College Station,TX.
Clark, D.N.,1980. The Diagenesis of Zechstein carbonate sediments.Contrib[J]. Sedimentol.9,167-203.
Davies G R, Smith L B. Structurally cont rolled hydrothermal dolomite reservoir facies:An overview [J]. AAPG Bulletin,2006,90(11):1641-1690.
H.L.Barnes.1979.热液矿床地球化学[M].北京：地质出版社,1985：7
Hans G. Machel, Jeff Lonnee. Hydrothermal dolomite-a product of poor definition and imagination. Sedimentary Geology[J],2002,152 (34):163-171
Kramm, U., Wedepohl, K.H.,1991. The isotopic composition of strontium and sulfur in seawater of Late Permian (Zechstein)age [J]. Chem. Geol.90, 253-262.
Krouse., H.R., Viau, C.A., Eliuk, L.S., Ueda, A., Halas, S.,1988. Chemical and isotopic evidence of thermochemical sulphate reduction by light hydrocarbon gases in deep carbonate reservoirs[J]. Nature 333,415-419.
Popp B N, Anderson T F, Sandberg P A. Textural, elemental, and isotopic variations among constituents in Middle Devonian limestones, North Ameriea[J]. Sediment Res,1986,56(5):715-727.
Rick Wierzbicki, Jeffrey J. Dravis. Burial dolomitizatization and dissolution of Upper Jurassic Abenaki platform carbonates, Deep Panuke reservoir, Nova Scotia, Canada [J]. AAPG Bulletin,2006,90(11):1843-1861.
Smith L B, Davies G R. Structurally controlled hydrothermal alteration of carbonate reservoirs:Introduction [J]. AAPG Bulletin,2006,90(11):1635-1640.
Smith L B. Origin and reservoir characteristics of upper Ordovician Trenton-black river hydrothermal dolomite reservoirs in New York[J]. AAPG Bulletin,2006, 90(11):1691-1718.
Veizer J, Demovic R. Strontium as a tool for facies analysis [J]. Journal of Sedimentary Petrology,1974,44:93-115.
Veizer J, Fritz P, Jones B. Geochemistry of brachiopods, oxygen and carbon isotopic records of Paleozoic oceans[J]. Geochim Cosmochim Acta,1986,50(8): 1679-1696.
Veizer, J., Ala, D., Azmy, K., Bruckschen, P., Buhl, D., Bruhn, F.,Carden, G.A.F., Diener, A., Ebneth, S., Godderis, Y., Jasper, T., Korte, C., Pawellek, F., Podlaha, O.G., Strauss, H.,1999.87Sr/86Sr,813C and δ180 evolution of Phanerozoic seawater [J]. Chem. Geol.161,59-88.
Zenger D H. Burial dolomitization in the Lost Burro Formation(Devonian), eastcentral California, and the significance of late diagenetic dolomitization [J]. Geology,1983,11(9):519-522.
陈汉林,贾成造,1997.塔里木盆地地质热事件研究[J].科学通报42(10)：1096-1099
邓胜徽,黄智斌,景秀春,等.塔里木盆地西部奥陶系内部不整合[J].地质论评54(6)：741-747
何莹,鲍志东,沈安江,等.塔里木盆地牙哈—英买力地区寒武系—下奥陶统白云岩形成机理[J].沉积学报,2006,24(6)：806-818.
胡受奚,叶瑛等.交代蚀变岩岩石学及找矿意义[M].北京：地质出版社,2004：3.
贾承造,魏国齐,姚惠君等,盆地构造演化与区域构造地质[M].北京：石油工业出版社1995：12
贾承造.中国塔里木盆地构造特征与油气[M].北京：石油工业出版社,1997：23
贾存善,马旭杰,饶丹,等.2007.塔河油田奥陶系油田水同位素特征及地质意义[J],石油实验地质,29(3)：292-297.
金之钧,张刘平,胡文瑄等,2002.沉积盆地深部流体的地球化学特征及油气成藏效应初探[J].地球科学-中国地质大学学报,27(6)：659-665
钱一雄,邹远荣,陈跃,等.塔里木盆地塔中西北部多期、多成因岩溶作用地质-地球化学表征—以中1井为例[J].沉积学报,2005,23(4)：596-603.
邵龙义,Jones T P.桂中晚二叠世碳酸盐岩碳同位素的地层学意义[J].沉积学报,1999,17(1)：84-88.
王安甲,初广震,黄文辉,等.2008.塔里木盆地奥陶系碳酸盐岩碳氧稳定同位素地球化学特征[J].成都理工大学学报(自然科学版),35(6)：700-704.
徐维胜,热液改造碳酸盐岩储层综合研究[J].内蒙古石油化工.2009,(1)：20-22.
张景廉,金之钧,等.2001.塔里木盆地深部地质流体与油气藏的关系.新疆石油地质,22(5)：371-375
张兴阳,张水昌,罗平,等.塔中地区晚燕山—喜马拉雅期油气调整与热液活动的关系[J].科学通报,2007,52(增1)：192-198.
张学丰,胡文,张军涛.白云岩成因相关问题及主要形成模式[J].地质科技情报,2006,25(5)：32-40.
周志毅.塔里木盆地各纪地层[M].北京：科学出版社,2001,35-102
朱金富,于炳松,黄文辉,等.塔里木盆地塔中地区晚寒武世—奥陶世碳酸盐岩碳、氧同位素特征[J].大庆石油地质与开发,2008,27(1)：40-42.
Adam J E, Rhodes M L. Dolomitization by seepage reflux[J]. AAPG Bulletin,1960, 44(12):1912-1920.
Badiozamani K. The dorag dolomitization model, application to the middle Ordovician of Wisconsin[J]. Journal of Sedimentary Research,1973,43(4): 965-984.
Boreen, T., and G. R. Davies,2004, Hydrothermal dolomite and leached limestones in a TCF gas play: The Ladyfern Slave Point reservoir, NEBC, in R. McAuley, ed., Dolomites-The spectrum: Mechanisms, models, reservoir development: Canadian Society of Petroleum Geologists, Seminar and Core Conference, January 13-15,2004, Calgary, Extended Abstracts, CD format.
Boreen, T., and K. Colquhoun,2001, Ladyfern, NEBC:Major gas discovery in the Devonian Slave Point Formation (abs.):Canadian Society of Petroleum Geologists, Annual Convention, Abstracts, p.112/1-5.
Bruckschen, P., S. Oesmann, and J. Veizer,1999, Isotope stratigraphy of the European Carboniferous:Proxy signals for ocean chemistry, climate and tectonics [J]. Chemical Geology, v.161,127-163.
Chow, N., Morad, S., Al-Asam, I.S.,1996. Origin of authigenic carbonates in Eocene to Quaternary sediments from the Artic Ocean and Norwegian-Greenland Sea[J]. Proc. Ocean Drilling Program Sci. Res., vol.151, pp.415-434.College Station,TX.
Clark, D.N.,1980. The Diagenesis of Zechstein carbonate sediments.Contrib[J]. Sedimentol.9,167-203.
Davies G R, Smith L B. Structurally cont rolled hydrothermal dolomite reservoir facies:An overview [J]. AAPG Bulletin,2006,90(11):1641-1690.
H.L.Barnes.1979.热液矿床地球化学[M].北京：地质出版社,1985：7
Hans G. Machel, Jeff Lonnee. Hydrothermal dolomite-a product of poor definition and imagination. Sedimentary Geology[J],2002,152 (34):163-171
Kramm, U., Wedepohl, K.H.,1991. The isotopic composition of strontium and sulfur in seawater of Late Permian (Zechstein)age [J]. Chem. Geol.90, 253-262.
Krouse., H.R., Viau, C.A., Eliuk, L.S., Ueda, A., Halas, S.,1988. Chemical and isotopic evidence of thermochemical sulphate reduction by light hydrocarbon gases in deep carbonate reservoirs[J]. Nature 333,415-419.
Popp B N, Anderson T F, Sandberg P A. Textural, elemental, and isotopic variations among constituents in Middle Devonian limestones, North Ameriea[J]. Sediment Res,1986,56(5):715-727.
Rick Wierzbicki, Jeffrey J. Dravis. Burial dolomitizatization and dissolution of Upper Jurassic Abenaki platform carbonates, Deep Panuke reservoir, Nova Scotia, Canada [J]. AAPG Bulletin,2006,90(11):1843-1861.
Smith L B, Davies G R. Structurally controlled hydrothermal alteration of carbonate reservoirs:Introduction [J]. AAPG Bulletin,2006,90(11):1635-1640.
Smith L B. Origin and reservoir characteristics of upper Ordovician Trenton-black river hydrothermal dolomite reservoirs in New York[J]. AAPG Bulletin,2006, 90(11):1691-1718.
Veizer J, Demovic R. Strontium as a tool for facies analysis [J]. Journal of Sedimentary Petrology,1974,44:93-115.
Veizer J, Fritz P, Jones B. Geochemistry of brachiopods, oxygen and carbon isotopic records of Paleozoic oceans[J]. Geochim Cosmochim Acta,1986,50(8): 1679-1696.
Veizer, J., Ala, D., Azmy, K., Bruckschen, P., Buhl, D., Bruhn, F.,Carden, G.A.F., Diener, A., Ebneth, S., Godderis, Y., Jasper, T., Korte, C., Pawellek, F., Podlaha, O.G., Strauss, H.,1999.87Sr/86Sr,813C and δ180 evolution of Phanerozoic seawater [J]. Chem. Geol.161,59-88.
Zenger D H. Burial dolomitization in the Lost Burro Formation(Devonian), eastcentral California, and the significance of late diagenetic dolomitization [J]. Geology,1983,11(9):519-522.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |