塔里木盆地寒武系碳酸盐岩层序地层特征
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摘要
运用碳酸盐岩层序地层学理论,通过野外露头观察、钻井资料分析及地震剖面综合解释技术,开展塔里木盆地下古生界碳酸盐岩层序地层研究,识别层序边界,建立地层格架。对塔里木盆地寒武系碳酸盐岩识别出的8个层序特征进行刻画,除层序SQ1为基准面上升半旋回型层序外,其他层序均为基准面下降半旋回型层序,其中层序SQ5,SQ6,SQ7,SQ8为重点勘探层序。在轮南地区,层序SQ6,SQ7,SQ8为今后构造-岩性复合圈闭重点勘探层序。建立了塔里木盆地寒武系碳酸盐岩层序发育模式,指出了有利于碳酸盐岩储层发育的层序样式,为寻找地层-岩性圈闭发育有利部位提供了依据。
Sequence stratigraphic theories of carbonate are employed in a sequence stratigraphic study on the Lower Paleozoic carbonates in Tarim Basin through outcrop observation,drilling data analysis as well as integra-ted seismic interpretations.Together with the study,the sequence boundaries are identified and stratigraphic framework is established.As a result,eight sequences identified in the Cambrian carbonates are described.Except for sequence 1(SQ 1) as a ascending base level semi-cycle sequence,the other sequences are all falling base level semi-cycle sequences.Sequences 5,6,7 and 8 are considered key hydrocarbon exploration targets.In Lunnan area,exploration activities shall be focused on sequences 6,7 and 8 for complex structural-lithologic traps.A model for the Cambrian carbonate sequences in the Tarim Basin is developed and provides helpful aid to searching for places with favorable conditions for the formation of stratigraphic lithologic traps.
Sequence stratigraphic theories of carbonate are employed in a sequence stratigraphic study on the Lower Paleozoic carbonates in Tarim Basin through outcrop observation,drilling data analysis as well as integra-ted seismic interpretations.Together with the study,the sequence boundaries are identified and stratigraphic framework is established.As a result,eight sequences identified in the Cambrian carbonates are described.Except for sequence 1(SQ 1) as a ascending base level semi-cycle sequence,the other sequences are all falling base level semi-cycle sequences.Sequences 5,6,7 and 8 are considered key hydrocarbon exploration targets.In Lunnan area,exploration activities shall be focused on sequences 6,7 and 8 for complex structural-lithologic traps.A model for the Cambrian carbonate sequences in the Tarim Basin is developed and provides helpful aid to searching for places with favorable conditions for the formation of stratigraphic lithologic traps.
引文
[1]威尔格斯C K.层序地层学原理(海平面变化综合分析)[M].徐怀大,魏魁生,洪卫东,等译.北京:石油工业出版社,1993:83-105.Wilgus C K.Principles of sequence stratigraphy(comprehensiveanalysis of sea-level change)[M].Transcated by Xu Huaida,Wei kuisheng,Hong weidong,et al.Beijing:Petroleum IndustryPress,1993:83-105.
[2]纪友亮.层序地层学[M].上海:同济大学出版社,2005:54-89.Ji Youliang.Sequence stratigraphy[M].Shanghai:Tongji Uni-versity Press,2005:54-89.
[3]许效松.层序地层学研究进展[J].岩相古地理,1994,14(1):34-39.Xu xiaosong.Advances in sequence stratigraphy[J].Sedimen-tary Facies and Palaeogeography,1994,14(1):34-39.
[4]吴因业,顾家裕.油气层序地层学[M].北京:石油工业出版社,2002:20-53.Wu Yinye,Gu Jiayu.Petroluem sequence stratigraphy[M].Beijing:Petroleum Industry Press,2002:20-53.
[5]Hunt D,Tucker M E.Stranded parasequences and the forcedregressive wedge systems tract deposition during base-level fall[J].Sedimentary Geology,1992,81:1-9.
[6]Sarg J F.Carbonate sequence stratigraphy[C]∥Wilgus C K,etal,eds.Sea level changes:an integrated approach.SEPM Spe-cial Publication,1988,42:155-181.
[7]Sloss L L.Forty years of sequence stratigraphy[J].GeologicalSociety of America Bulletin,1988,100(11):1661-1665.
[8]Mitchum R M Jr,Van W J C.High-frequency sequence andtheir stacking pattern:sequence-stratigraphic evidence of high-frequency eustatic cycles[J].Sedimentary Geology,1991,70:131-160.
[9]Vail P R,Mitchum R M,Thompson S.Seismic stratigrphy andgloble changes of sea level[J].AAPG Memoir,1997,26:63-97.
[10]Galloway W.Genetic stratigraphic sequences in basin analysis(1):architecture and genesis of flooding surface bounded de-positional units[J].AAPG Bulletin,1989,73(2):125-142.
[11]Cross T A.Stratigraphic controls on reservoir attributes in conti-nental strata[J].Earth Sciences Frontiers,2000,7(4):322-350.
[12]Wilson J L.Carbonate facies in geologic history[M].NewYork:Springer,1975:471.
[13]冯增昭,彭勇民,金振奎,等.中国寒武纪和奥陶纪岩相古地理[M].北京:石油工业出版社,2004:123-124.Feng zhenzhao,Peng yongmin,Jin Zhenkui,et al.Lithofacies pa-leogeography of the Cambrian and Ordovician in China[M].Beijing:Petroleum Industry Press,2004:123-124.
[14]张师本,倪寓南,龚福华,等.塔里木盆地周缘地层考察指南[M].北京:石油工业出版社,2003:9-16.Zhang Shiben,Ni Yunan,Gong Fuhua,et al.A guide to thestratigraphic investigation on the periphery of the Tarim Basin[M].Beijing:Petroleum Industry Press,2003:9-16.
[15]徐怀大,樊太亮,韩革华,等.新疆塔里木盆地层序地层特征[M].北京:地质出版社,1997:166-191.Xu Huaida,Fan Tailiang,Han Gehua,et al.Sequence pattern ofthe Tarim basin,Xinjiang[M].Beijing:Geological PublishingHouse,1997:166-191.
[16]漆立新,云露.塔河油田奥陶系碳酸盐岩岩溶发育特征与主控因素[J].石油与天然气地质,2010,31(1):1-12.Qi Lixin,Yun Lu.Development characteristics and main con-trolling factors of the Ordovician carbonate karst in Tahe oilfield[J].Oil&Gas Geolog,2010,31(1):1-12.
[17]云露,翟晓先.塔里木盆地塔深1井寒武系储层与成藏特征探讨[J].石油与天然气地质,2008,29(6):726-732.Yun Lu,Zhai Xiaoxian.Discussion on characteristics of theCambrian reservoirs and hydrocarbon accumulation in wellTashen-1,Tarim Basin[J].Oil&Gas Geolog,2008,29(6):726-732.
[18]李慧莉,钱一雄,沙旭光,等.塔里木盆地卡塔克隆起西北倾没端良里塔格组碳酸盐岩储层发育特征与影响因素[J].石油与天然气地质,2010,31(1):69-77.Li Huilin,Qian Yixiong,Sha Xuguang,et al.Development char-acteristics and influencing factors of carbonate reservoirs in theOrdovician Lianglitage Formation at the northwest pitching endof the Katake Uplift,the Tarim Basin[J].Oil&Gas Geolog,2010,31(1):69-77.
[2]纪友亮.层序地层学[M].上海:同济大学出版社,2005:54-89.Ji Youliang.Sequence stratigraphy[M].Shanghai:Tongji Uni-versity Press,2005:54-89.
[3]许效松.层序地层学研究进展[J].岩相古地理,1994,14(1):34-39.Xu xiaosong.Advances in sequence stratigraphy[J].Sedimen-tary Facies and Palaeogeography,1994,14(1):34-39.
[4]吴因业,顾家裕.油气层序地层学[M].北京:石油工业出版社,2002:20-53.Wu Yinye,Gu Jiayu.Petroluem sequence stratigraphy[M].Beijing:Petroleum Industry Press,2002:20-53.
[5]Hunt D,Tucker M E.Stranded parasequences and the forcedregressive wedge systems tract deposition during base-level fall[J].Sedimentary Geology,1992,81:1-9.
[6]Sarg J F.Carbonate sequence stratigraphy[C]∥Wilgus C K,etal,eds.Sea level changes:an integrated approach.SEPM Spe-cial Publication,1988,42:155-181.
[7]Sloss L L.Forty years of sequence stratigraphy[J].GeologicalSociety of America Bulletin,1988,100(11):1661-1665.
[8]Mitchum R M Jr,Van W J C.High-frequency sequence andtheir stacking pattern:sequence-stratigraphic evidence of high-frequency eustatic cycles[J].Sedimentary Geology,1991,70:131-160.
[9]Vail P R,Mitchum R M,Thompson S.Seismic stratigrphy andgloble changes of sea level[J].AAPG Memoir,1997,26:63-97.
[10]Galloway W.Genetic stratigraphic sequences in basin analysis(1):architecture and genesis of flooding surface bounded de-positional units[J].AAPG Bulletin,1989,73(2):125-142.
[11]Cross T A.Stratigraphic controls on reservoir attributes in conti-nental strata[J].Earth Sciences Frontiers,2000,7(4):322-350.
[12]Wilson J L.Carbonate facies in geologic history[M].NewYork:Springer,1975:471.
[13]冯增昭,彭勇民,金振奎,等.中国寒武纪和奥陶纪岩相古地理[M].北京:石油工业出版社,2004:123-124.Feng zhenzhao,Peng yongmin,Jin Zhenkui,et al.Lithofacies pa-leogeography of the Cambrian and Ordovician in China[M].Beijing:Petroleum Industry Press,2004:123-124.
[14]张师本,倪寓南,龚福华,等.塔里木盆地周缘地层考察指南[M].北京:石油工业出版社,2003:9-16.Zhang Shiben,Ni Yunan,Gong Fuhua,et al.A guide to thestratigraphic investigation on the periphery of the Tarim Basin[M].Beijing:Petroleum Industry Press,2003:9-16.
[15]徐怀大,樊太亮,韩革华,等.新疆塔里木盆地层序地层特征[M].北京:地质出版社,1997:166-191.Xu Huaida,Fan Tailiang,Han Gehua,et al.Sequence pattern ofthe Tarim basin,Xinjiang[M].Beijing:Geological PublishingHouse,1997:166-191.
[16]漆立新,云露.塔河油田奥陶系碳酸盐岩岩溶发育特征与主控因素[J].石油与天然气地质,2010,31(1):1-12.Qi Lixin,Yun Lu.Development characteristics and main con-trolling factors of the Ordovician carbonate karst in Tahe oilfield[J].Oil&Gas Geolog,2010,31(1):1-12.
[17]云露,翟晓先.塔里木盆地塔深1井寒武系储层与成藏特征探讨[J].石油与天然气地质,2008,29(6):726-732.Yun Lu,Zhai Xiaoxian.Discussion on characteristics of theCambrian reservoirs and hydrocarbon accumulation in wellTashen-1,Tarim Basin[J].Oil&Gas Geolog,2008,29(6):726-732.
[18]李慧莉,钱一雄,沙旭光,等.塔里木盆地卡塔克隆起西北倾没端良里塔格组碳酸盐岩储层发育特征与影响因素[J].石油与天然气地质,2010,31(1):69-77.Li Huilin,Qian Yixiong,Sha Xuguang,et al.Development char-acteristics and influencing factors of carbonate reservoirs in theOrdovician Lianglitage Formation at the northwest pitching endof the Katake Uplift,the Tarim Basin[J].Oil&Gas Geolog,2010,31(1):69-77.
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