煤系地层成煤环境及层序地层研究
|
摘要
以先进的层序地层学、高分辨率层序地层序、沉积学等理论和方法为指导,以青海省石炭纪～侏罗纪含煤地层为研究对象,开展了沉积体系、岩相古地理、层序地层、聚煤规律及其控制因素研究。
通过对研究区野外剖面系统、细致的观察,结合测井、地震及区域资料的综合分析,应用宏观和微观相结合的手段,在岩石类型、沉积构造、剖面结构分析的基础上,在研究区石炭纪～侏罗纪识别出2个沉积体系组、11个沉积相,详细论述了各类沉积体系特征。在上述基础上,针对成煤沉积体系进行了深入系统的研究,并建立了冲积扇-扇三角洲成煤环境、曲流河-曲流河三角洲成煤环境、辫状河-辫状河三角洲成煤环境、湖泊成煤环境及有障壁海岸成煤环境成煤模式。
针对不同的沉积体系类型,采用不同的层序地层学理论和技术方法开展含煤层序地层研究。石炭纪～三叠纪含煤地层为海相沉积地层,运用Vail经典层序地层学的方法,通过基干剖面研究,在层序界面特征、界面的成因类型研究的基础上,建立了层序划分方案,详细讨论了各级层序特征;中下侏罗统含煤地层为陆相沉积地层,运用高分辨率层序地层学进行研究,从中识别出短期、中期、长期3个级别的基准面旋回层序,进一步分析各级次旋回层序特征。在此基础上,详细研究煤层在层序地层格架中发育规律。
在成煤环境、成煤模式及层序地层研究的基础上,结合前人研究成果,对青海省4个赋煤带进行煤炭资源量预测,其中祁连山赋煤带煤炭预测资源量为2205650万吨、柴北缘赋煤带煤炭预测资源量为1207787万吨、唐古拉赋煤带煤炭预测资源量为532557万吨,东昆仑-西秦岭赋煤带煤炭预测资源量为54006万吨。在上述基础上进行靶区优选,包括大通矿区外围找煤靶区、宁缠矿区外围找煤靶区、聚乎更矿区西段找煤靶区、滩间山找煤靶区、鱼卡煤田东部找煤靶区、野马滩—军牧场找煤靶区、结扎找煤靶区、豹草沟—尕松山找煤靶区、开心岭找煤靶区及扎苏-达哈找煤靶区等10个找靶区。
Base on sequence stratigraphy, high-resolution sequence , sedimentary and other theories and methods, the depositional system, lithofacies palaeogeography, coal-accumulating and controlling factors of Carboniferous-Jurassic in Qinghai Province have been studied.
Two group sedimentary facies, eleven sedimentary facies and many subfacies, microfacies types have been recognized and the depositional models have been stablished by macroscopical and microcosmic research methods, basing on the detailedly observation of field profile, combinated with conventional log, seismic and regional geological condition. Based on previous analysis, the coal-forming environments were systematical researched. The coal-forming patterns of alluvial fan—fan delta system, meandering river- meandering-delta, and braided-braided delta have been established.
It is necessary to consider multiple factors in sequence analyses and to apply different interpretation models for different types of coal-forming environment. The coal - bearing strata of Carboniferous- Triassic is marine strata . Base on anlysis sequence boundaries and interface generation, the sequence stratigraphy framework is built up and the characteristics of the sequences are analyzed by Vail classic sequence theories and methods. The coal - bearing strata of Middle - Lower Jurassic Series is continental formation. Combined with the high resolution sequence stratigraphic theory, The formation was divided into short-term ,middle-term and long-term base-level cycle. On base of the previous analysis, the coal development pattern in sequence stratigraphic framework was analysised.
Based on the comprehensive analysis of coal-forming environment, coal-forming pattern, and sequence stratigraphy, makes use of results of predecessors, the four enriched regularit ies of coal in Qinghai Province have been predicted, which include 22.05656 billion tons of coal resources in Qilian Mts, 12.07787 billion tons of coal resource in migration of north Qaidam Basin, 5.32557 billion tons of coal resource in Tanggula Mts, 0.54006 billion tons of coal resources in East Kunlun- West Qinling Mts. On the base of the study, the ten target areas have been predicted, which include the target area of Datong Mining Area outside, the target area of Ningchan Mining Area outside, the target area of Juhugeng Mining Area outside, the target area of Tanjian Mts Mining Area outside, the target area of Eastern of Yuqia , the target area of Yematan—Junmuchang, the target area of Jiezha, the target area of Baocaogou—gasong Mts, the target area of Kaixinling, and the target area of Zhasu—daha.
通过对研究区野外剖面系统、细致的观察,结合测井、地震及区域资料的综合分析,应用宏观和微观相结合的手段,在岩石类型、沉积构造、剖面结构分析的基础上,在研究区石炭纪～侏罗纪识别出2个沉积体系组、11个沉积相,详细论述了各类沉积体系特征。在上述基础上,针对成煤沉积体系进行了深入系统的研究,并建立了冲积扇-扇三角洲成煤环境、曲流河-曲流河三角洲成煤环境、辫状河-辫状河三角洲成煤环境、湖泊成煤环境及有障壁海岸成煤环境成煤模式。
针对不同的沉积体系类型,采用不同的层序地层学理论和技术方法开展含煤层序地层研究。石炭纪～三叠纪含煤地层为海相沉积地层,运用Vail经典层序地层学的方法,通过基干剖面研究,在层序界面特征、界面的成因类型研究的基础上,建立了层序划分方案,详细讨论了各级层序特征;中下侏罗统含煤地层为陆相沉积地层,运用高分辨率层序地层学进行研究,从中识别出短期、中期、长期3个级别的基准面旋回层序,进一步分析各级次旋回层序特征。在此基础上,详细研究煤层在层序地层格架中发育规律。
在成煤环境、成煤模式及层序地层研究的基础上,结合前人研究成果,对青海省4个赋煤带进行煤炭资源量预测,其中祁连山赋煤带煤炭预测资源量为2205650万吨、柴北缘赋煤带煤炭预测资源量为1207787万吨、唐古拉赋煤带煤炭预测资源量为532557万吨,东昆仑-西秦岭赋煤带煤炭预测资源量为54006万吨。在上述基础上进行靶区优选,包括大通矿区外围找煤靶区、宁缠矿区外围找煤靶区、聚乎更矿区西段找煤靶区、滩间山找煤靶区、鱼卡煤田东部找煤靶区、野马滩—军牧场找煤靶区、结扎找煤靶区、豹草沟—尕松山找煤靶区、开心岭找煤靶区及扎苏-达哈找煤靶区等10个找靶区。
Base on sequence stratigraphy, high-resolution sequence , sedimentary and other theories and methods, the depositional system, lithofacies palaeogeography, coal-accumulating and controlling factors of Carboniferous-Jurassic in Qinghai Province have been studied.
Two group sedimentary facies, eleven sedimentary facies and many subfacies, microfacies types have been recognized and the depositional models have been stablished by macroscopical and microcosmic research methods, basing on the detailedly observation of field profile, combinated with conventional log, seismic and regional geological condition. Based on previous analysis, the coal-forming environments were systematical researched. The coal-forming patterns of alluvial fan—fan delta system, meandering river- meandering-delta, and braided-braided delta have been established.
It is necessary to consider multiple factors in sequence analyses and to apply different interpretation models for different types of coal-forming environment. The coal - bearing strata of Carboniferous- Triassic is marine strata . Base on anlysis sequence boundaries and interface generation, the sequence stratigraphy framework is built up and the characteristics of the sequences are analyzed by Vail classic sequence theories and methods. The coal - bearing strata of Middle - Lower Jurassic Series is continental formation. Combined with the high resolution sequence stratigraphic theory, The formation was divided into short-term ,middle-term and long-term base-level cycle. On base of the previous analysis, the coal development pattern in sequence stratigraphic framework was analysised.
Based on the comprehensive analysis of coal-forming environment, coal-forming pattern, and sequence stratigraphy, makes use of results of predecessors, the four enriched regularit ies of coal in Qinghai Province have been predicted, which include 22.05656 billion tons of coal resources in Qilian Mts, 12.07787 billion tons of coal resource in migration of north Qaidam Basin, 5.32557 billion tons of coal resource in Tanggula Mts, 0.54006 billion tons of coal resources in East Kunlun- West Qinling Mts. On the base of the study, the ten target areas have been predicted, which include the target area of Datong Mining Area outside, the target area of Ningchan Mining Area outside, the target area of Juhugeng Mining Area outside, the target area of Tanjian Mts Mining Area outside, the target area of Eastern of Yuqia , the target area of Yematan—Junmuchang, the target area of Jiezha, the target area of Baocaogou—gasong Mts, the target area of Kaixinling, and the target area of Zhasu—daha.
引文
[1]邵震杰、任文忠、陈家良,煤田地质学,北京:煤炭工业出版社,1993
[2]杨起,韩德馨,中国煤田地质学(上册),北京:煤炭工业出版社,1979
[3]钱大都,魏斌贤,李钰,等.中国煤炭资源总论.北京:地质出版社,1996
[4]青海省煤田资源预测与评价(第三次煤田预测)[R].青海煤田地质勘探公司.1994,110-238.
[5]张承兆.柴达木盆地煤炭资源及其开发潜力分析[J].中国煤田地质,1997,9(2):78-79.
[6]Van Wagoner,J.C.,Overview of sequence stratigraphy of forland basin deposites:summary of papers,and glossary of sequence stratigraphy[A].In:J.C.Van wagoner and G.T.Bertran(edtors),Sequence stratigraphy of forlandBasin deposits-outcrop and Subsuface.Examples from the Cretaceous of north America[C].Am.Assoc.Pet.Geol.,Mem.,1995 a 64:Ⅸ-Ⅻ.
[7]Potonie H,Koorders S H Sumpftlachmoor nature der moore des produktiven carbons Jahrb der kon preusz.Geology Lan-desanstalt,Berlin,1909.
[8]Theissen R.The constitution of coal.Transactions of the America Institute of Mining and Metallogeny.1925.
[9]彭格林,张则有,伍大茂.泥炭与煤形成环境对比研究现状[J].地球科学进展,1999,14(3):247-255.
[10]魏钦廉,伊海生,肖玲.陆源碎屑岩中的古土壤在地层分析中的应用[J].古地理学报,2006,8(2):211-219
[11]刘光华.煤沉积学研究现状与动态[J].地学前缘,1999,6(增刊):101-110
[12]Diessel C F G.Coal-bearing Lkpositiona! Systems.Vew York:Springer-Verlag,1992.721[1]
[13]Vail P R.Sea-level changes during the Paleozoic[J].Oceans,1979,22(1):23-25
[14]Vail P R.Seismic stratigraphy interpretation using sequence stratigraphy.Part 1:Seismic stratigraphy interpretation procedure.In:Bally A W,ed.Atlas of Seismic stratigraphy.American Association of petroleum Geologists,Studies in Geology,1987,27:1-10
[15]Cross T A.and Lessenger M A.Sediment volume partitioning:rationale for stratigraphic model evolution and high-resolution stratigraphic correlation.Gradstein FM,Sandvik K O,Milton NJ.Sequence Stratigraphic Concepts and Applications.NPF Special Publication,1998,12(8):171-195
[16]Cross T A.and Lessenger,Sediment Volume Partitioning:Rationale for Stratigraphic Model Evaluation and High-Resolution Stratigraphic Correlation,Accepted for publication in Norwegian Petroleums Forening Conference Volume,1996
[17]Cross T A,Maker M R,et al.Applications of High-resolution Sequence Stratigraphy to Reservoir Analysis[J].Proceed aligns of the 7th Exploration and Production Research Conference,Paris Wechnip,1993,45(1):11-33
[18]邵龙义,张鹏飞.论幕式聚煤作用及含煤岩系层序地层学研究[A].见:顾家裕等主编.层序地层学及其在油气勘探开发中的应用论文集[C].北京:石油工业出版社,1997,124-128.
[19]邵龙义,张鹏飞.含煤岩系层序地层模式[J].长春科技大学学报(专辑),1998,67-72.
[20]邵龙义,陈家良,李瑞军,等.广西合山二叠世碳酸盐岩型煤系层序地层分析[J].沉积学报,2003,21(1):168-174.
[21]Longyi Shao,Pengfei Zhang,R.A.Gayer,jialiang Chen&Shifeng Dai.Coal in a carbonate sequence stratigraphic framework:the Upper Permian Heshan Formation in central Guangxi,southern China[J].Journal of the Geological Society,London,2003,160:285-298.
[22]邵龙义,张鹏飞,窦建伟,等.含煤岩系层序地层分析的新认识[J].中国矿业大学,1999,28(1)20-24.
[23]吴因业.煤层-一种陆相盆地中的成因层序边界[J].石油学报,1996,17(4):28-35
[24]Posamentier,H.W.& James,D.C.,An overview of sequence-stratigraphic cincepts:uses and abuses[A].In:Posamentier,H.W.,Summerhayes,C.P.,Haq,B.U.,&Allen,G.P.,(eds).Sequence straigraphy and facies associations[C].International Associaation of Sedimentologists,Special Publication,1993,77:731-742.
[25]Posamentier,H.W.&Weimer,P.,Siliciclastic sequence stratigraphy and petroleum gelogy-where to from here?[J]American Association of Petroleum Geologist Bulletin,1993,77:731-742.
[26]Miall,A.D.,Exxon global-cycle chart:aneventfor every occasion[J].Geology,1992.20:787-790.
[27]Gibling M R,Bird D J.Late Carboniferous cyclothems and alluvial paleovalleys in the Sydney Basin,Nova Scotia.GeolSoc Am gull,1994,106:105-117
[28]Cobb J C,Ceeil C B.Modem and ancient coal forming environments.Geol Soc Spec Pap,1993,286:1-198.
[29]Raseldine R S.Coals reviewed:depositional controls,modem analogues and ancient climates.In.Whately M K G,Pickering K T,eds.Delta:Sites and Trnps for Fossil Fuels.Gaol Soc London Spec Publ.1989,41:289-309
[30]Heckel P H.Glacial-ecstatic base-level-climatic model for late Middle to Late Pennsylvanian coal-bed formation in the Appalachian Basin.Journal of Sedimentary Resazrch,Section B:Stratigraphy and Global Studies,1995,B65(3):348-356
[31]Liu Guanghua.Petmo-Carboniferous paleogeography and coal accumulation and their tectonic control in the North and South continental plates.Internat J Gxil Genl,1990,16:73-117
[32]Ralhmani R A,Flores F Reds.Sedimentology of coal and coal-bearing sequences.Internal Assoc of Sedimentologists Special paper,1984,7:1-412
[33]Scott.A.C,ed.Coal and coal-bearirta strata:recent advances.GeolSoc Speacial Publication,1987,32:1-332
[34]邵龙义,刘红梅,田宝霖.上扬子地区晚二叠代沉积演化与聚煤[J].沉积学报,1998,19(2):54-60.
[35]李增学,王明镇,余继峰,等.鄂尔多斯盆地晚古生代含煤地层层序地层与海侵成煤特点[J].沉积学报,2006,24(6):834-840
[36]李增学,余继峰,郭建斌,等.陆表海盆地海侵事件成煤作用机制分析[J].沉积学报,2003,21(2):288-297.
[37]李增学,魏久传,韩美莲.鲁西陆表海盆地高分辨率层序划分与海侵过程成煤特点[J].沉积学报,2000,18(3):362-368.
[38]杨明慧,夏文臣.非海相前陆盆地含煤沉积层序地层分析-以柴达木盆地大煤沟侏罗系剖面为例[J].煤田地质与勘探,1998,26(3):1-5.
[39]杨永泰,张宝民,席萍,等.柴达木盆地北缘侏罗系层序地层与沉积相研究[J].地学前缘(中国地质大学,北京),2000,7(3):155-159.
[40]彭立才,杨慧珠.柴达木盆地大煤沟侏罗系剖面高分辨率含煤层系分析[J].西安石油学院 学报(自然科学版).2000,17(1):6-10.
[41]刘天绩.柴北缘柴达木盆地北缘侏罗系煤炭资源形成条件研究及资源评价[D].北京:中国矿业大学,博士论文,2006.
[42]尹成明,江波,韩秦鹏等.柴达木盆地石油勘探潜力及勘探方向[J].中国石油勘探,2006,6,68-41.
[43]文怀军,鲁静,尚潞君,等.青海聚乎更矿区侏罗纪含煤岩系层序地层研究[J].中国煤田地质,2006,18(5):19-21.
[44]许靖华,大地构造与沉积作用[M].北京:地质出版社,1985
[45]万天丰,朱鸿.东亚大陆各陆块中新生代运动学特征研究[A].岩石圈构造与动力学开放研究室1995年年报[C].北京:地质出版社,1996,19-29.
[46]黄克兴,夏玉成.构造控煤概论[M].北京:煤炭出版社,1991
[47]青海省地质矿产局.青海省区域地质志[M].北京:地质出版社,1991.
[48]王煦曾,朱榔如,王杰,著.中国煤田的形成与演化[M].科学出版社,1992,83-86.
[49]杨起等,华北石炭二叠纪煤变质特征与地质因素探讨[M].北京:地质出版社,1988
[50]张泓等,中国西北侏罗纪含煤地层与聚煤规律[M].北京:地质出版社,1998
[51]吴传荣,张慧,李远虑,等.西北早-中侏罗世煤岩煤质与煤变质研究[M].北京:煤炭工业出版社,1995
[52]刘宝珺,曾允孚.岩相古地理基础和工作方法[M].北京:地质出版社,1985.
[52]邬金华,余素玉.一个湖泊一三角洲沉积总体中泥质岩成因地层研究的元素统计分析[J].沉积学报,1996,14(1):59-68.
[54]朱有光,李泽九,胡以铿.区域地球化学异常系统评价的思路与方法[J].地质科技情报,1997,16(2):97-103.
[55]邓宏文,钱凯.试论湖相泥质岩的地球化学二分性[J].石油与天然气地质,1993,14(2):85-97.
[56]蔡忠贤,贾振远.碳酸盐台地三级层序界面的讨论[J].地球科学,1997,V22(5):456-459;
[57]许效松,刘宝珺等.上扬子西缘二叠纪一三叠纪层序地层与盆山转换耦合[M].北京:地质出版社,1997.
[58]张占松.测井资料识别层序的方法及问题讨论[J].石油勘探与开发,2000,027(005):119-121.
[59]黄思静.上扬子台地区晚古生代海相碳酸盐岩的碳、锶同位素研究[J].地质学报,1997.V71(1):P45-53
[60]黄思静,石和.上扬子石炭一二叠纪海相碳酸盐的锶同位素演化与全球海平面变化[J].沉积学报,2001,V19(4):481-487
[61]田景春,曾允孚.中国南方二叠纪古海洋锶同位素演化[J].沉积学报,1995,V12(1):40-44
[62]Vail P R.Seismic stratigraphy interpretation using sequence stratigraphy.Part 1:Seismic stratigraphy interpretation procedure.In:Bally A W,ed.Atlas of Seismic stratigraphy.American Association of petroleum Geologists,Studies in Geology,1987,27:1-10
[63]Johnson J G,Klapper G,Sandberg C A.Devonian eustatic fluctuations in Euramerica[J].Bulletin American Association Petroleum Geologists,1982,99(6):567-587
[64]Galloway W E.Genetic stratigraphic sequences in basin analysis[J].AAPG Bulletin,1989,73(1):125-154
[65]邓宏文,王洪亮,李熙吉.层序地层基准面的识别、对比技术及应用[J].石油与天然气地质,1996,17(3):177-184
[66]邓宏文,王洪亮,翟爱军,等.中国陆源碎屑盆地层序地层与储层展布[J].石油与天然气地质,1999,20(2):108-114
[67]郑荣才,彭军,吴朝容.陆相盆地基准面旋同的级次划分和研究意义[J].沉积学报,2001,19(2):249-255
[68]黄克兴,夏玉成.构造控煤概论.北京:煤炭出版社,1991
[69]许靖华,大地构造与沉积作用,北京:地质出版社,1985
[70]朱志澄,逆冲推覆构造,武汉:中国地质大学出版社,1991
[71]胡受权,曹运江,等.柴达木盆地侏罗纪盆地原型及其形成与演化探讨[J].石油实验地质,1999,21(3):189-195.
[72]汤良杰,金之钧,张明利,等.柴达木盆地构造古地理分析[J].地学前缘(中国地质大学,北京),2000,7(4):421-429.
[73]郑孟林,李明杰,曹春潮,等.柴达木北缘西段侏罗纪盆地构造特征与演化[J].石油实验地质,2004,26(4):315-323.
[74]伍跃中,陈守康,等.青海省控煤因素简析[J].中国煤田地质,1997,9(4):10-13
[75]曾联波,金之钧,张明利,等.柴达木侏罗纪盆地性质及其演化特征[J].沉积学报,2002,20(2):288-292.
[76]田景瑞,大地构造运动与成煤原理,北京:地震出版社,1992
[77]张韬,中国主要聚煤期沉积环境与聚煤规律,北京:地质出版社,1995
[78]张鹏飞,彭苏萍,邵龙义等编著.含煤岩系沉积环境分析.北京:煤炭工业出版社,1993
[79]鲁静,邵龙义,刘天绩,等.柴北缘鱼卡地区侏罗纪含煤地层层序地层学研究[J].煤田地质与勘探,2007,35(1):1-6.
[80]王仁农、李桂春,中国含煤盆地演化和聚煤规律,北京:煤炭工业出版社 1998
[81]陈毓川等,中国主要成矿区带矿产资源远景评价,北京:地质出版社,1999
[82]陈毓川等著,中国成矿体系与区域成矿评价(上、下册),北京:地质出版社2007
[83]陶长辉、徐榜荣、史振亚等,煤田普查与勘探,徐州:中国矿业大学出版社,1988
[84]田三岗等,煤炭资源评价探析,太原:山西科学技术出版社,1999.
[2]杨起,韩德馨,中国煤田地质学(上册),北京:煤炭工业出版社,1979
[3]钱大都,魏斌贤,李钰,等.中国煤炭资源总论.北京:地质出版社,1996
[4]青海省煤田资源预测与评价(第三次煤田预测)[R].青海煤田地质勘探公司.1994,110-238.
[5]张承兆.柴达木盆地煤炭资源及其开发潜力分析[J].中国煤田地质,1997,9(2):78-79.
[6]Van Wagoner,J.C.,Overview of sequence stratigraphy of forland basin deposites:summary of papers,and glossary of sequence stratigraphy[A].In:J.C.Van wagoner and G.T.Bertran(edtors),Sequence stratigraphy of forlandBasin deposits-outcrop and Subsuface.Examples from the Cretaceous of north America[C].Am.Assoc.Pet.Geol.,Mem.,1995 a 64:Ⅸ-Ⅻ.
[7]Potonie H,Koorders S H Sumpftlachmoor nature der moore des produktiven carbons Jahrb der kon preusz.Geology Lan-desanstalt,Berlin,1909.
[8]Theissen R.The constitution of coal.Transactions of the America Institute of Mining and Metallogeny.1925.
[9]彭格林,张则有,伍大茂.泥炭与煤形成环境对比研究现状[J].地球科学进展,1999,14(3):247-255.
[10]魏钦廉,伊海生,肖玲.陆源碎屑岩中的古土壤在地层分析中的应用[J].古地理学报,2006,8(2):211-219
[11]刘光华.煤沉积学研究现状与动态[J].地学前缘,1999,6(增刊):101-110
[12]Diessel C F G.Coal-bearing Lkpositiona! Systems.Vew York:Springer-Verlag,1992.721[1]
[13]Vail P R.Sea-level changes during the Paleozoic[J].Oceans,1979,22(1):23-25
[14]Vail P R.Seismic stratigraphy interpretation using sequence stratigraphy.Part 1:Seismic stratigraphy interpretation procedure.In:Bally A W,ed.Atlas of Seismic stratigraphy.American Association of petroleum Geologists,Studies in Geology,1987,27:1-10
[15]Cross T A.and Lessenger M A.Sediment volume partitioning:rationale for stratigraphic model evolution and high-resolution stratigraphic correlation.Gradstein FM,Sandvik K O,Milton NJ.Sequence Stratigraphic Concepts and Applications.NPF Special Publication,1998,12(8):171-195
[16]Cross T A.and Lessenger,Sediment Volume Partitioning:Rationale for Stratigraphic Model Evaluation and High-Resolution Stratigraphic Correlation,Accepted for publication in Norwegian Petroleums Forening Conference Volume,1996
[17]Cross T A,Maker M R,et al.Applications of High-resolution Sequence Stratigraphy to Reservoir Analysis[J].Proceed aligns of the 7th Exploration and Production Research Conference,Paris Wechnip,1993,45(1):11-33
[18]邵龙义,张鹏飞.论幕式聚煤作用及含煤岩系层序地层学研究[A].见:顾家裕等主编.层序地层学及其在油气勘探开发中的应用论文集[C].北京:石油工业出版社,1997,124-128.
[19]邵龙义,张鹏飞.含煤岩系层序地层模式[J].长春科技大学学报(专辑),1998,67-72.
[20]邵龙义,陈家良,李瑞军,等.广西合山二叠世碳酸盐岩型煤系层序地层分析[J].沉积学报,2003,21(1):168-174.
[21]Longyi Shao,Pengfei Zhang,R.A.Gayer,jialiang Chen&Shifeng Dai.Coal in a carbonate sequence stratigraphic framework:the Upper Permian Heshan Formation in central Guangxi,southern China[J].Journal of the Geological Society,London,2003,160:285-298.
[22]邵龙义,张鹏飞,窦建伟,等.含煤岩系层序地层分析的新认识[J].中国矿业大学,1999,28(1)20-24.
[23]吴因业.煤层-一种陆相盆地中的成因层序边界[J].石油学报,1996,17(4):28-35
[24]Posamentier,H.W.& James,D.C.,An overview of sequence-stratigraphic cincepts:uses and abuses[A].In:Posamentier,H.W.,Summerhayes,C.P.,Haq,B.U.,&Allen,G.P.,(eds).Sequence straigraphy and facies associations[C].International Associaation of Sedimentologists,Special Publication,1993,77:731-742.
[25]Posamentier,H.W.&Weimer,P.,Siliciclastic sequence stratigraphy and petroleum gelogy-where to from here?[J]American Association of Petroleum Geologist Bulletin,1993,77:731-742.
[26]Miall,A.D.,Exxon global-cycle chart:aneventfor every occasion[J].Geology,1992.20:787-790.
[27]Gibling M R,Bird D J.Late Carboniferous cyclothems and alluvial paleovalleys in the Sydney Basin,Nova Scotia.GeolSoc Am gull,1994,106:105-117
[28]Cobb J C,Ceeil C B.Modem and ancient coal forming environments.Geol Soc Spec Pap,1993,286:1-198.
[29]Raseldine R S.Coals reviewed:depositional controls,modem analogues and ancient climates.In.Whately M K G,Pickering K T,eds.Delta:Sites and Trnps for Fossil Fuels.Gaol Soc London Spec Publ.1989,41:289-309
[30]Heckel P H.Glacial-ecstatic base-level-climatic model for late Middle to Late Pennsylvanian coal-bed formation in the Appalachian Basin.Journal of Sedimentary Resazrch,Section B:Stratigraphy and Global Studies,1995,B65(3):348-356
[31]Liu Guanghua.Petmo-Carboniferous paleogeography and coal accumulation and their tectonic control in the North and South continental plates.Internat J Gxil Genl,1990,16:73-117
[32]Ralhmani R A,Flores F Reds.Sedimentology of coal and coal-bearing sequences.Internal Assoc of Sedimentologists Special paper,1984,7:1-412
[33]Scott.A.C,ed.Coal and coal-bearirta strata:recent advances.GeolSoc Speacial Publication,1987,32:1-332
[34]邵龙义,刘红梅,田宝霖.上扬子地区晚二叠代沉积演化与聚煤[J].沉积学报,1998,19(2):54-60.
[35]李增学,王明镇,余继峰,等.鄂尔多斯盆地晚古生代含煤地层层序地层与海侵成煤特点[J].沉积学报,2006,24(6):834-840
[36]李增学,余继峰,郭建斌,等.陆表海盆地海侵事件成煤作用机制分析[J].沉积学报,2003,21(2):288-297.
[37]李增学,魏久传,韩美莲.鲁西陆表海盆地高分辨率层序划分与海侵过程成煤特点[J].沉积学报,2000,18(3):362-368.
[38]杨明慧,夏文臣.非海相前陆盆地含煤沉积层序地层分析-以柴达木盆地大煤沟侏罗系剖面为例[J].煤田地质与勘探,1998,26(3):1-5.
[39]杨永泰,张宝民,席萍,等.柴达木盆地北缘侏罗系层序地层与沉积相研究[J].地学前缘(中国地质大学,北京),2000,7(3):155-159.
[40]彭立才,杨慧珠.柴达木盆地大煤沟侏罗系剖面高分辨率含煤层系分析[J].西安石油学院 学报(自然科学版).2000,17(1):6-10.
[41]刘天绩.柴北缘柴达木盆地北缘侏罗系煤炭资源形成条件研究及资源评价[D].北京:中国矿业大学,博士论文,2006.
[42]尹成明,江波,韩秦鹏等.柴达木盆地石油勘探潜力及勘探方向[J].中国石油勘探,2006,6,68-41.
[43]文怀军,鲁静,尚潞君,等.青海聚乎更矿区侏罗纪含煤岩系层序地层研究[J].中国煤田地质,2006,18(5):19-21.
[44]许靖华,大地构造与沉积作用[M].北京:地质出版社,1985
[45]万天丰,朱鸿.东亚大陆各陆块中新生代运动学特征研究[A].岩石圈构造与动力学开放研究室1995年年报[C].北京:地质出版社,1996,19-29.
[46]黄克兴,夏玉成.构造控煤概论[M].北京:煤炭出版社,1991
[47]青海省地质矿产局.青海省区域地质志[M].北京:地质出版社,1991.
[48]王煦曾,朱榔如,王杰,著.中国煤田的形成与演化[M].科学出版社,1992,83-86.
[49]杨起等,华北石炭二叠纪煤变质特征与地质因素探讨[M].北京:地质出版社,1988
[50]张泓等,中国西北侏罗纪含煤地层与聚煤规律[M].北京:地质出版社,1998
[51]吴传荣,张慧,李远虑,等.西北早-中侏罗世煤岩煤质与煤变质研究[M].北京:煤炭工业出版社,1995
[52]刘宝珺,曾允孚.岩相古地理基础和工作方法[M].北京:地质出版社,1985.
[52]邬金华,余素玉.一个湖泊一三角洲沉积总体中泥质岩成因地层研究的元素统计分析[J].沉积学报,1996,14(1):59-68.
[54]朱有光,李泽九,胡以铿.区域地球化学异常系统评价的思路与方法[J].地质科技情报,1997,16(2):97-103.
[55]邓宏文,钱凯.试论湖相泥质岩的地球化学二分性[J].石油与天然气地质,1993,14(2):85-97.
[56]蔡忠贤,贾振远.碳酸盐台地三级层序界面的讨论[J].地球科学,1997,V22(5):456-459;
[57]许效松,刘宝珺等.上扬子西缘二叠纪一三叠纪层序地层与盆山转换耦合[M].北京:地质出版社,1997.
[58]张占松.测井资料识别层序的方法及问题讨论[J].石油勘探与开发,2000,027(005):119-121.
[59]黄思静.上扬子台地区晚古生代海相碳酸盐岩的碳、锶同位素研究[J].地质学报,1997.V71(1):P45-53
[60]黄思静,石和.上扬子石炭一二叠纪海相碳酸盐的锶同位素演化与全球海平面变化[J].沉积学报,2001,V19(4):481-487
[61]田景春,曾允孚.中国南方二叠纪古海洋锶同位素演化[J].沉积学报,1995,V12(1):40-44
[62]Vail P R.Seismic stratigraphy interpretation using sequence stratigraphy.Part 1:Seismic stratigraphy interpretation procedure.In:Bally A W,ed.Atlas of Seismic stratigraphy.American Association of petroleum Geologists,Studies in Geology,1987,27:1-10
[63]Johnson J G,Klapper G,Sandberg C A.Devonian eustatic fluctuations in Euramerica[J].Bulletin American Association Petroleum Geologists,1982,99(6):567-587
[64]Galloway W E.Genetic stratigraphic sequences in basin analysis[J].AAPG Bulletin,1989,73(1):125-154
[65]邓宏文,王洪亮,李熙吉.层序地层基准面的识别、对比技术及应用[J].石油与天然气地质,1996,17(3):177-184
[66]邓宏文,王洪亮,翟爱军,等.中国陆源碎屑盆地层序地层与储层展布[J].石油与天然气地质,1999,20(2):108-114
[67]郑荣才,彭军,吴朝容.陆相盆地基准面旋同的级次划分和研究意义[J].沉积学报,2001,19(2):249-255
[68]黄克兴,夏玉成.构造控煤概论.北京:煤炭出版社,1991
[69]许靖华,大地构造与沉积作用,北京:地质出版社,1985
[70]朱志澄,逆冲推覆构造,武汉:中国地质大学出版社,1991
[71]胡受权,曹运江,等.柴达木盆地侏罗纪盆地原型及其形成与演化探讨[J].石油实验地质,1999,21(3):189-195.
[72]汤良杰,金之钧,张明利,等.柴达木盆地构造古地理分析[J].地学前缘(中国地质大学,北京),2000,7(4):421-429.
[73]郑孟林,李明杰,曹春潮,等.柴达木北缘西段侏罗纪盆地构造特征与演化[J].石油实验地质,2004,26(4):315-323.
[74]伍跃中,陈守康,等.青海省控煤因素简析[J].中国煤田地质,1997,9(4):10-13
[75]曾联波,金之钧,张明利,等.柴达木侏罗纪盆地性质及其演化特征[J].沉积学报,2002,20(2):288-292.
[76]田景瑞,大地构造运动与成煤原理,北京:地震出版社,1992
[77]张韬,中国主要聚煤期沉积环境与聚煤规律,北京:地质出版社,1995
[78]张鹏飞,彭苏萍,邵龙义等编著.含煤岩系沉积环境分析.北京:煤炭工业出版社,1993
[79]鲁静,邵龙义,刘天绩,等.柴北缘鱼卡地区侏罗纪含煤地层层序地层学研究[J].煤田地质与勘探,2007,35(1):1-6.
[80]王仁农、李桂春,中国含煤盆地演化和聚煤规律,北京:煤炭工业出版社 1998
[81]陈毓川等,中国主要成矿区带矿产资源远景评价,北京:地质出版社,1999
[82]陈毓川等著,中国成矿体系与区域成矿评价(上、下册),北京:地质出版社2007
[83]陶长辉、徐榜荣、史振亚等,煤田普查与勘探,徐州:中国矿业大学出版社,1988
[84]田三岗等,煤炭资源评价探析,太原:山西科学技术出版社,1999.