豫西上、下石盒子组（P_（2-3））沉积旋回特征及聚煤环境
|
摘要
本论文在总结前人所做工作的基础之上,依据野外露头、测井、岩芯等资料,搜集了平顶山12-20钻孔资料以及其他专著、文献资料,选取禹州大风口、济源下冶两个野外露头作为实测剖面,结合露头、钻井和测试分析资料,综合研究了沉积体系、沉积类型、沉积相、沉积亚相及沉积微相的特征,划分了上、下石盒子组基准面旋回层序,推断基准面升降规律,总结旋回特征,编制上、下石盒子组地层等厚线图、砂地比等厚线图,并绘制出岩相古地理图,在此基础上探讨豫西上、下石盒子组聚煤环境。
运用现代沉积学理论,较详细分析了豫西地区上、下石盒子组沉积相、沉积亚相和沉积微相的特征,按沉积亚相划分了沉积类型,建立了十七种沉积类型,包括上三角洲平原8种,下三角洲平原7种,三角洲前缘2种。同时绘制了豫西禹州大风口、平顶山12-20钻孔以及济源下冶地区三地区上、下石盒子组地层柱状图、相柱状图各1幅。
将基准面旋回理论应用到豫西上、下石盒子组对该地层进行层序地层划分,分别对平顶山12-20钻孔、禹州大风口和济源下冶三地区的中期、短期基准面层序地层进行划分,识别了平顶山12-20中期基准面旋回8个,均为对称旋回;41个短期旋回,其中对称短期旋回为20个,非对称短期旋回21个,非对称短期旋回以向上变深的退积为主,向上变浅的加积旋回不发育;识别了大风口剖面中期旋回7个,其中对称旋回6个,非对称旋回1个,为向上变浅的半旋回,短期旋回共23个,其中对称旋回为10个,非对称旋回13个,有向上变深和向上变浅的两种非对称旋回;下冶地区识别了4个中期旋回,其中3个为对称旋回,一个为向上变深的非对称旋回,14个短期旋回,其中对称的短期旋回7个,非对称短期旋回7个。并分别探讨了各个地区的中期基准面旋回过程中的短期基准面结构类型的变化和叠置关系。
绘制了河南省上、下石盒子组地层等厚线图、砂地比等值线图各1幅,并通过相比法绘制了上、下石盒子组的岩相古地理图。在豫西的中部地区为下三角洲平原,由于分流河道分叉增多且分流间湾发育,只形成一些不稳定薄煤层,仅局部达可采厚度。而在本区南部,三角洲分流间湾变得较开阔,充填淤平后可形成面积较大的分流间沼泽。局部废弃的三角洲朵体上以及广阔的海湾边缘环境也有利于聚煤作用的广泛发育,形成的煤层层数多,厚度大,且较稳定。研究区的聚煤环境主要是分流间湾泥炭沼泽,泥炭坪聚煤环境不发育,随着三角洲不断向前推进,聚煤作用的范围也随之增大。
Based on the work done by our predecessors, and relying on the materal of the outcrops, well logging, cores, etc., selecting two outcrops, which are Dafengkou inYuzhou and xiaye in Jiyuan, as the measured profile, collecting data of drilling 12-20 in Pingdingshan, as well as other monographs、references, combining the information of outcrops, drillings and testing analysis, this paper has a comprehensive study on the characteristics of the sedimentary system, deposit types, sedimentary facies, sedimentary subfacies and microfacies, and divides the base-level cyclic sequences in the Upper and Lower Shihezi Formations, infers the lifting rules of base-level, review the cycle characteristics, draws out stratigraphic isopach map and sand-mud ratio contour map of the strata and the lithofacies palaeogeography maps, on this basis the coal-accumulating environment of the upper and lower Shihezi Formations in west Henan has been discussed.
With the theory of modern sedimentation, this paper has a detailed analysis on features of sedimentary facies, sedimentary subfacies and microfacies in west Henan, divides the sediment types based on the sedimentary subfacies, including eight types of the upper delta plain, seven kinds of the lower delta plain, three kinds of the delta front. Then the stratigraphic column and formation phase histogram of the Upper and Lower Shihezi Formations in Dafengkou of Yuzhou city, drilling 12-20 of Pingdingshan city, xiaye area of Jiyuan city were drawed respectively.
Applied the base-level cycles to the division of sequence stratigraphy of the Upper and Lower Shihezi Formations in western Henan, the medium-term, short-term base-level sequence formation are divided respectively in drilling 12-20 of Pingdingshan, Dafengkou of Yuzhou and xiaye of Jiyuan. 8 medium-term base-level cycles are identified in Pingdingshan 12-20, all symmetrical cycle; 41 short-term cycles, in which 20 symmetrical and 21 asymmetrical, non-symmetrical short-term cycles were mainly retrogradation in order to darken up, any shallowing-upward aggradational cycle was not development; 7 mid-cycles are identified in profile of Dafengkou, in which 6 symmetrical cycles, 1 asymmetric cycle, the half-cycles of upward shallowing, short-term cycles of 23 Among them, 10 symmetrical cycles and 13 non-symmetric cycles, there are two kinds of non-symmetric cycles which includes upward shallowing ones and upward darker ones; 4 medium-term cycles are identified in Xiaye area, in which 3 symmetrical cycles, 1 asymmetric cycle, the half-cycles of upward shallowing, 14 short-term cycles, including seven symmetrical short-term cycles, 7 non-symmetrical short-term cycles.The changement and Superimposition of structural type of the short-term base-level cycles in the process of medium-term base-level in various regions respectivelyhave been Explored.
The stratigraphic isopach map, Sand-mud ratio contour map on Upper and Lower Shihezi Formations in Henan Province have been drawn, and lithofacies palaeogeography maps on the strata with facies-comparation method. It was a lower delta plain in the central region of west Henan, due to an increased bifurcation of distributary channel and the development of interdistributary, only some unstable thin coal seams which only can be taken up partially were formed. In the south of this area, the interdistributary became broader, formed larger stream swamp after filling with silt level. Locally abandoned delta body, as well as the edge of the vast bay environment, is also conducive to the extensive development of coal accumulation, the multi-layered coal seams formed are thick, and more stable. It tells that the coal-accumulating environment of the study area should primarily be deltic interdistributary peat bog, peat flat is not developed, with the delta continue to move forward, the scope of coal accumulation is even greater.
运用现代沉积学理论,较详细分析了豫西地区上、下石盒子组沉积相、沉积亚相和沉积微相的特征,按沉积亚相划分了沉积类型,建立了十七种沉积类型,包括上三角洲平原8种,下三角洲平原7种,三角洲前缘2种。同时绘制了豫西禹州大风口、平顶山12-20钻孔以及济源下冶地区三地区上、下石盒子组地层柱状图、相柱状图各1幅。
将基准面旋回理论应用到豫西上、下石盒子组对该地层进行层序地层划分,分别对平顶山12-20钻孔、禹州大风口和济源下冶三地区的中期、短期基准面层序地层进行划分,识别了平顶山12-20中期基准面旋回8个,均为对称旋回;41个短期旋回,其中对称短期旋回为20个,非对称短期旋回21个,非对称短期旋回以向上变深的退积为主,向上变浅的加积旋回不发育;识别了大风口剖面中期旋回7个,其中对称旋回6个,非对称旋回1个,为向上变浅的半旋回,短期旋回共23个,其中对称旋回为10个,非对称旋回13个,有向上变深和向上变浅的两种非对称旋回;下冶地区识别了4个中期旋回,其中3个为对称旋回,一个为向上变深的非对称旋回,14个短期旋回,其中对称的短期旋回7个,非对称短期旋回7个。并分别探讨了各个地区的中期基准面旋回过程中的短期基准面结构类型的变化和叠置关系。
绘制了河南省上、下石盒子组地层等厚线图、砂地比等值线图各1幅,并通过相比法绘制了上、下石盒子组的岩相古地理图。在豫西的中部地区为下三角洲平原,由于分流河道分叉增多且分流间湾发育,只形成一些不稳定薄煤层,仅局部达可采厚度。而在本区南部,三角洲分流间湾变得较开阔,充填淤平后可形成面积较大的分流间沼泽。局部废弃的三角洲朵体上以及广阔的海湾边缘环境也有利于聚煤作用的广泛发育,形成的煤层层数多,厚度大,且较稳定。研究区的聚煤环境主要是分流间湾泥炭沼泽,泥炭坪聚煤环境不发育,随着三角洲不断向前推进,聚煤作用的范围也随之增大。
Based on the work done by our predecessors, and relying on the materal of the outcrops, well logging, cores, etc., selecting two outcrops, which are Dafengkou inYuzhou and xiaye in Jiyuan, as the measured profile, collecting data of drilling 12-20 in Pingdingshan, as well as other monographs、references, combining the information of outcrops, drillings and testing analysis, this paper has a comprehensive study on the characteristics of the sedimentary system, deposit types, sedimentary facies, sedimentary subfacies and microfacies, and divides the base-level cyclic sequences in the Upper and Lower Shihezi Formations, infers the lifting rules of base-level, review the cycle characteristics, draws out stratigraphic isopach map and sand-mud ratio contour map of the strata and the lithofacies palaeogeography maps, on this basis the coal-accumulating environment of the upper and lower Shihezi Formations in west Henan has been discussed.
With the theory of modern sedimentation, this paper has a detailed analysis on features of sedimentary facies, sedimentary subfacies and microfacies in west Henan, divides the sediment types based on the sedimentary subfacies, including eight types of the upper delta plain, seven kinds of the lower delta plain, three kinds of the delta front. Then the stratigraphic column and formation phase histogram of the Upper and Lower Shihezi Formations in Dafengkou of Yuzhou city, drilling 12-20 of Pingdingshan city, xiaye area of Jiyuan city were drawed respectively.
Applied the base-level cycles to the division of sequence stratigraphy of the Upper and Lower Shihezi Formations in western Henan, the medium-term, short-term base-level sequence formation are divided respectively in drilling 12-20 of Pingdingshan, Dafengkou of Yuzhou and xiaye of Jiyuan. 8 medium-term base-level cycles are identified in Pingdingshan 12-20, all symmetrical cycle; 41 short-term cycles, in which 20 symmetrical and 21 asymmetrical, non-symmetrical short-term cycles were mainly retrogradation in order to darken up, any shallowing-upward aggradational cycle was not development; 7 mid-cycles are identified in profile of Dafengkou, in which 6 symmetrical cycles, 1 asymmetric cycle, the half-cycles of upward shallowing, short-term cycles of 23 Among them, 10 symmetrical cycles and 13 non-symmetric cycles, there are two kinds of non-symmetric cycles which includes upward shallowing ones and upward darker ones; 4 medium-term cycles are identified in Xiaye area, in which 3 symmetrical cycles, 1 asymmetric cycle, the half-cycles of upward shallowing, 14 short-term cycles, including seven symmetrical short-term cycles, 7 non-symmetrical short-term cycles.The changement and Superimposition of structural type of the short-term base-level cycles in the process of medium-term base-level in various regions respectivelyhave been Explored.
The stratigraphic isopach map, Sand-mud ratio contour map on Upper and Lower Shihezi Formations in Henan Province have been drawn, and lithofacies palaeogeography maps on the strata with facies-comparation method. It was a lower delta plain in the central region of west Henan, due to an increased bifurcation of distributary channel and the development of interdistributary, only some unstable thin coal seams which only can be taken up partially were formed. In the south of this area, the interdistributary became broader, formed larger stream swamp after filling with silt level. Locally abandoned delta body, as well as the edge of the vast bay environment, is also conducive to the extensive development of coal accumulation, the multi-layered coal seams formed are thick, and more stable. It tells that the coal-accumulating environment of the study area should primarily be deltic interdistributary peat bog, peat flat is not developed, with the delta continue to move forward, the scope of coal accumulation is even greater.
引文
[1] Rahmani R A.Facies control of gas trapping.Lower Cretaceous Falher A cycle,Elnrworth area,Northwestern Alberta[J].AAPG,1984:115-140
[2]陈钟惠,《煤和含煤岩系的沉积环境》[M]。北京:中国地质大学出版社,1988年
[3]张鹏飞,彭苏萍,邵龙义等.含煤岩系沉积环境分析[M].煤炭工业出版社,1993年
[4] Udden J A . Geology and mineral resources of the Peoria quadrangle, Illinois[J].U.S.Geol.Surv.Bull.,1912,506:103
[5] Weller J M.Cyclic sedimentation of the Pennsylvanian period and its significance[J].Journal of Geology,1930,38:97-135
[6] Wanless H R,Shepard F P.Sea level and climatic changes related to Late Paleozoic cycles[J] .Geol.Soc.Amer.Bull.,1936,47:1117-1206
[7] Wanless H R , Weller J M . Correlation and extent of Pennsylvanian cyclothems[J].Geo1.Soc.Amer.Bul1.,1932,43:1003—1016.
[8] Fisk H N.Recent Mississippi River sedimentation and peat accumulation,Compte Rendu du Quat.Congr.Pour l'avancement des Etudes de Strat.et de Geo1.du Carbonifere Heerlen,1960,Sept:15—20,187—199.
[9] Ferm J C.Depositional models in coal exploration and developmen[C].In:Sasena R S(ed).Sedimentary environments and hydrocarbans.AAPG/NOGS short course,New Orleans Geological Society,1976,60—78
[10] Coleman J.M. and Prior D.B.Deltaic environment spiculiles as shoreline indicators in deltaic sequence ,in Geol.Soc.Amer.Bull. 1982,Vol79,200-272
[11] Horne J C,Ferm J C,Caruccio,et a1.Depositional models coal exploration and mine planning in Appalachian region[J].American Association of Petroleum Geologists Bulletin,1978,62:2 3792 411
[12] Vail P R. Mitchum R M .Todd R G Widmier J M. Thompson S Sagree J B. Bubb J N. Hatlelid W G.Seismic stratigraphy and global changes of sea-level [A].In:Payton C.E.(ed.),Seismic stratigraphy applications to hydrocarbon exploration.AAGP Memoir,1977,(26):49-211
[13] Posamentier H W,et al.Eustatic controls on clastic deposition I—conceptual framework,in C K Wilgus et al eds.Sea level changes:An integrated approach.SEPM special publication,1988,Vol.42
[14] Mitchum R M Jr and Van Wagoner J C.High-Frequency Sequences and their stacking patterns:Sequence-stratigraphy evidence of high-frequency eustatic cycles.Sediment.Geol,1991,70:131-164
[15] Mitchum R M Jr Vail P R and Thompson S.Seismic stratigraphy and global changes of sea level , part2 : the depositional sequence as a basic unit for stratigraphic analysis.In:C.E.Payton(eds),Seismic stratigraphy-Application to Hydrocarbon Exploration. Am.Assoc.Pet.Geol.Mem.,1977,26:213-248
[16] Posamentier H W Jervey M T﹠Vail P R.Eustatic controls on clastic deposition I-conceptual framework.In:Wilgus,C.K.,Hastings,B.S.,Kendall,C.G.St.C., Posamentier,H.W.,Ross,C.A.﹠Van Wagoner,J.C.(eds),Sea-level changes:an integerated approach.Society of Economic Palaeontologists and Mineralogists,Special Publication,1988,42:109-124
[17] Vail P R Mitchum R M Todd R G Widmier J M Thompson S Sagree J B Bubb J N Hatlelid W G.Seismic stratigraphy and global changes of sea-level [A].In:Payton C.E.(ed.),Seismic stratigraphy applications to hydrocarbon exploration.AAGP Memoir,1977,(26):49-211
[18] Vail P R Mitchum R M﹠Thompson S.Seismic stratigraphy and global changes of sea-level.Part4.Global cycles of relative changes of sea-level[A].In : Payton , C.E.( eds ) ,Seismic stratigraphy-applications to hydrocarbon exploration.American Association of Petroleum Geologists,Memoir,26:83-98
[19] Van Wagoner J C,Mitchum R M,Campion K M’and Rahmanian V D.Siliciclastic sequence Stratigraphy in well logs, cores ,and outcrops: Concepts for high-resolution corelation of time and facies.Am.Assoc.Pet.Geol..Methods in exploration series,1990,7:55
[20] Sloss L L,W C Krumbein and E C Dapples.Integrated facies analysis, in C R Longwell ed.Sedimentary facies geologic history:Geological Society of American Memoir,1949,Vol.39
[21] Sloss L L.Sequence in the Cratonic interior of North America. Geological society of American.Bulletin,1963,Vol.74
[22] Wilgus C K Posamentier H W Hastings B S.《层序地层学原理(海平面变化综合分析)》[M].北京:石油出版社,1993
[23] Loutit T S et al..Condensed sections:the key to age determination and correlation of continental margin sequences,in C.K. Wilgus et al eds.Sea level changes:an integrated approach.SEPM special publication,1988,Vol.42
[24] Lingdsay J F.Sequence stratigraphy and Depositional controls in Late Proterozoic-Early Cambrian sedinents of Amadeus Basin.Central Australia.AAGP Bulleltin,1987,Vol.71,No.11
[25] Christie—Blick N et al.Sequence stratigraphy in Proterozoic successions.Geology,1988,Vol.16,No.2
[26] Dibona P A等著,熊兴武译.南澳大利亚费林德斯山脉晚元古代Wonoka组盆地—斜坡序列的演化与层序地层学.地质科学译丛,第四期
[27] Woodcock N H.Sequence stratigraphy of the Palaeozoic Welsh Basin..Journal of the Geological society,1990,Vol.147
[28] Prave A R..Depositional and Sequence stratigraphic framework of the Lower Cambrian Zabriskie Quartzite : Implications for regional correlation and the Early Cambrian paleogeography of the Death Valley region of Califoria and Nevada.Geological Society of American Bulletin, 1991,Vol.104,No.5
[29] Aiger T and G H Bachmann.Sequence stratigraphic framework of the Triassic.German。Sedimentary geology,1992,Vol.80
[30]乔秀夫,高林志.北京西山寒武系层序地层[J].中国地质科学院地质研究所所刊,1990,第22号,地质出版社
[31]孟祥华,葛铭.华北地台早古生代层序地层学及构造演化[J].“七五”地质科技重要成果学术交流会议论文选集.北京科学技术出版社,1992
[32]张川波,文琼英,汪筱林.克拉通边缘盆地碳酸盐层序地层学分析—以uhuabei板块东部早古生代沉积为例[J].长春地质学院学报,1993,23(4)
[33]陆彦邦等.安徽两淮地区奥陶纪层序地层海平面变化[J].安徽地质,1993,3(3)
[34]冯增昭,王英华,刘焕杰.中国沉积学[M].北京:石油工业出版社,1994年:1-896
[35]关士聪等.中国海陆变迁海域沉积相与油气[M].北京:科学出版社,1984.1-104
[36]王鸿祯.中国古地理图集[M].北京:地图出版社,1985:41-130
[37]刘宝珺曾允孚.岩相古地理基础与工作方法[M].地质出版社,1985年
[38]刘焕杰著.准格尔煤田含煤建造岩相古地理学研究[M].出版:地质出版社, 1991
[39]唐开疆.华北陆台晚古生代岩相古地理[J].沉积学报,1989,7(4):97-104
[40]盛吉虎、张恩惠.河南省早二叠世早期岩相古地理及聚煤作用研究[J].河南地质,1997,15(3):186-191
[41]许效松.古地理研究的前景与挑战[J].古地理学报,1999,1(4):1-11
[42]魏怀习.华北晚古生代煤系古地理演化[J].中国煤田地质,2001,13(4):14-15
[43]徐振永,王延斌等.沁水盆地晚古生代煤系层序地层及岩相古地理研究[J].煤田地质与勘探,2007,35(4):5-8
[44]蒋维红,董春梅等.岩相古地理研究现状及发展趋势[J].断块油气田,2007,14(3):1-3
[45]吴根耀.造山带古地理学——重建区域构造古地理的若干思考[J].古地理学报,2007,9(6):635-650
[46]朱如凯、许怀先.中国北方地区二叠纪岩相古地理[J].古地理学报,2007,9(2):133-142
[47]阎存凤、袁剑英、赵应成.被祁连东部石炭纪岩相古地理[J].沉积学报,2008,26(2):193-201
[48]陈晋镳、武铁山.全国地层多重划分对比研究10——华北区区域地层[M].武汉:中国地质大学出版社,1997,65-81
[49]河南省地质矿产局.河南省区域地质志[M].北京:地质出版社,1989,205-215
[50]张海清、李进化等.河南省地层古生物研究第四分册——晚古生代(华北型)[M].郑州:黄河水利出版社,2008,17-26
[51]辛仁臣,李桂范,王平在.河南永城地区上古生界沉积体系及其演化规律分析[J].黑龙江矿业学院学报,1996,6(12):11—18
[52]李文前,刘国志.豫东地区晚古生界聚煤规律研究[J].中国矿业,2008,17(6):58-61
[53]刘光华.河南禹县上石盒子组第六、七煤段沉积环境与聚煤特点[J].地质论评,1984,30(5)446-456
[54]江西煤田地质勘探公司、龚绍礼.河南禹县早二叠世晚期浅水三角洲沉积和聚煤环境[J].煤田地质,1986,1-8
[55]尹国勋.禹县煤田二叠系三煤段沉积环境与三9煤找煤方向[J].焦作矿业学院学报,1987,2:45-55
[56]翟玉琛.豫西登封煤田暴雨山井田上石盒子组第四含煤段沉积环境及聚煤特征[J].湘潭矿业学院学报,1991,6(2):112-116
[57]王果寿、裴振洪等.豫西地区中、下二叠统沉积特征[J].天然气工业,2003,23(6):24-29
[58]孙国忠、李永高.禹州市白庙矿含煤地层沉积环境及聚煤特征分析[J].中国煤炭地质,2008,20(增刊):19-21
[59]杨起.《河南禹县晚古生代煤系沉积环境与聚煤特征》[M].北京:地质出版社,1987,1-234
[60]郭熙年、唐仲林、李万程等.《河南省晚古生代聚煤规律》[M].武汉:中国地质大学出版社,1991年,1-321
[61]席文祥、裴放.《河南省岩石地层》[M].武汉:中国地质大学出版社,1997,116-148
[62]杨关秀.《中国豫西二叠纪华夏植物群——禹州植物群》[M].北京:地质出版社,2006,1-375
[63]王仁农.豫东二叠系[J].中国矿业学院学报,1982,2:50-60
[64]张士,焦清典.Lingula化石在嵩箕地区上石盒子组大量出现及其意义[J].煤田地质与勘探,1991,1:17-19
[65]王果寿、裴振洪等.豫西地区中、下二叠统沉积特征[J].天然气工业,2003,23(6):24-27
[66]魏魁生,徐怀大,叶淑蓉等.松辽盆地白垩系高分辨率层序地层格架[J].石油与天然气地质,1997,18(1):4-7
[67]吴朝容,郑荣才.辽河油田西部洼陷抄河街组高分辨率层序地层学特征[J].成都理工学院学报,1999,26(4):375-381
[68]邓宏文,王洪亮.李小孟.高分辨率层序地层对比在河流相中的应用[J].石油与天然气地质,1997,18(2):90-95
[69]王洪亮,邓宏文.地层基准面原理在胡相储层预测中的应用[J].石油与天然气地质,1997.18(2):96～102
[70]邓宏文,徐长费,王洪亮.陆东凹陷上侏罗统层序地层与生储盖组台[J].石油与天然气地质,1998,19(4):275-279
[71]郑荣才,吴朝容.西部凹陷辣层抄河街组生储盖组台的层序分析[J].成都理工学院学报,1999,26(4):348-356
[72]郑荣才,尹世民,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3):369-375
[73]郑荣才.四川盆地下侏罗统大安寨段高分辨率层序地层学特征[J].沉积学报,1998,16(2):42-49
[74]吴朝容,郑荣才.辽河油田西部洼陷抄河街组高分辨率层序地层学特征[J].成都理工学院学报,1999,26(4):375-381
[75]柳梅青,陈亦军,郑荣才.川西新场气田蓬莱镇组陆相地层高分辨率层序地层学研究[J].沉积学报,2000,18(1):50-56
[76]林万智等.中超板块晚古生代的古地磁特征[J].物探与化探,1984,5
[77]刘育燕,杨巍然,森永速男等.华北陆块、秦岭地块和扬子陆块构造演化的古地磁证据[J].地质科技情报,1993,12(4)
[2]陈钟惠,《煤和含煤岩系的沉积环境》[M]。北京:中国地质大学出版社,1988年
[3]张鹏飞,彭苏萍,邵龙义等.含煤岩系沉积环境分析[M].煤炭工业出版社,1993年
[4] Udden J A . Geology and mineral resources of the Peoria quadrangle, Illinois[J].U.S.Geol.Surv.Bull.,1912,506:103
[5] Weller J M.Cyclic sedimentation of the Pennsylvanian period and its significance[J].Journal of Geology,1930,38:97-135
[6] Wanless H R,Shepard F P.Sea level and climatic changes related to Late Paleozoic cycles[J] .Geol.Soc.Amer.Bull.,1936,47:1117-1206
[7] Wanless H R , Weller J M . Correlation and extent of Pennsylvanian cyclothems[J].Geo1.Soc.Amer.Bul1.,1932,43:1003—1016.
[8] Fisk H N.Recent Mississippi River sedimentation and peat accumulation,Compte Rendu du Quat.Congr.Pour l'avancement des Etudes de Strat.et de Geo1.du Carbonifere Heerlen,1960,Sept:15—20,187—199.
[9] Ferm J C.Depositional models in coal exploration and developmen[C].In:Sasena R S(ed).Sedimentary environments and hydrocarbans.AAPG/NOGS short course,New Orleans Geological Society,1976,60—78
[10] Coleman J.M. and Prior D.B.Deltaic environment spiculiles as shoreline indicators in deltaic sequence ,in Geol.Soc.Amer.Bull. 1982,Vol79,200-272
[11] Horne J C,Ferm J C,Caruccio,et a1.Depositional models coal exploration and mine planning in Appalachian region[J].American Association of Petroleum Geologists Bulletin,1978,62:2 3792 411
[12] Vail P R. Mitchum R M .Todd R G Widmier J M. Thompson S Sagree J B. Bubb J N. Hatlelid W G.Seismic stratigraphy and global changes of sea-level [A].In:Payton C.E.(ed.),Seismic stratigraphy applications to hydrocarbon exploration.AAGP Memoir,1977,(26):49-211
[13] Posamentier H W,et al.Eustatic controls on clastic deposition I—conceptual framework,in C K Wilgus et al eds.Sea level changes:An integrated approach.SEPM special publication,1988,Vol.42
[14] Mitchum R M Jr and Van Wagoner J C.High-Frequency Sequences and their stacking patterns:Sequence-stratigraphy evidence of high-frequency eustatic cycles.Sediment.Geol,1991,70:131-164
[15] Mitchum R M Jr Vail P R and Thompson S.Seismic stratigraphy and global changes of sea level , part2 : the depositional sequence as a basic unit for stratigraphic analysis.In:C.E.Payton(eds),Seismic stratigraphy-Application to Hydrocarbon Exploration. Am.Assoc.Pet.Geol.Mem.,1977,26:213-248
[16] Posamentier H W Jervey M T﹠Vail P R.Eustatic controls on clastic deposition I-conceptual framework.In:Wilgus,C.K.,Hastings,B.S.,Kendall,C.G.St.C., Posamentier,H.W.,Ross,C.A.﹠Van Wagoner,J.C.(eds),Sea-level changes:an integerated approach.Society of Economic Palaeontologists and Mineralogists,Special Publication,1988,42:109-124
[17] Vail P R Mitchum R M Todd R G Widmier J M Thompson S Sagree J B Bubb J N Hatlelid W G.Seismic stratigraphy and global changes of sea-level [A].In:Payton C.E.(ed.),Seismic stratigraphy applications to hydrocarbon exploration.AAGP Memoir,1977,(26):49-211
[18] Vail P R Mitchum R M﹠Thompson S.Seismic stratigraphy and global changes of sea-level.Part4.Global cycles of relative changes of sea-level[A].In : Payton , C.E.( eds ) ,Seismic stratigraphy-applications to hydrocarbon exploration.American Association of Petroleum Geologists,Memoir,26:83-98
[19] Van Wagoner J C,Mitchum R M,Campion K M’and Rahmanian V D.Siliciclastic sequence Stratigraphy in well logs, cores ,and outcrops: Concepts for high-resolution corelation of time and facies.Am.Assoc.Pet.Geol..Methods in exploration series,1990,7:55
[20] Sloss L L,W C Krumbein and E C Dapples.Integrated facies analysis, in C R Longwell ed.Sedimentary facies geologic history:Geological Society of American Memoir,1949,Vol.39
[21] Sloss L L.Sequence in the Cratonic interior of North America. Geological society of American.Bulletin,1963,Vol.74
[22] Wilgus C K Posamentier H W Hastings B S.《层序地层学原理(海平面变化综合分析)》[M].北京:石油出版社,1993
[23] Loutit T S et al..Condensed sections:the key to age determination and correlation of continental margin sequences,in C.K. Wilgus et al eds.Sea level changes:an integrated approach.SEPM special publication,1988,Vol.42
[24] Lingdsay J F.Sequence stratigraphy and Depositional controls in Late Proterozoic-Early Cambrian sedinents of Amadeus Basin.Central Australia.AAGP Bulleltin,1987,Vol.71,No.11
[25] Christie—Blick N et al.Sequence stratigraphy in Proterozoic successions.Geology,1988,Vol.16,No.2
[26] Dibona P A等著,熊兴武译.南澳大利亚费林德斯山脉晚元古代Wonoka组盆地—斜坡序列的演化与层序地层学.地质科学译丛,第四期
[27] Woodcock N H.Sequence stratigraphy of the Palaeozoic Welsh Basin..Journal of the Geological society,1990,Vol.147
[28] Prave A R..Depositional and Sequence stratigraphic framework of the Lower Cambrian Zabriskie Quartzite : Implications for regional correlation and the Early Cambrian paleogeography of the Death Valley region of Califoria and Nevada.Geological Society of American Bulletin, 1991,Vol.104,No.5
[29] Aiger T and G H Bachmann.Sequence stratigraphic framework of the Triassic.German。Sedimentary geology,1992,Vol.80
[30]乔秀夫,高林志.北京西山寒武系层序地层[J].中国地质科学院地质研究所所刊,1990,第22号,地质出版社
[31]孟祥华,葛铭.华北地台早古生代层序地层学及构造演化[J].“七五”地质科技重要成果学术交流会议论文选集.北京科学技术出版社,1992
[32]张川波,文琼英,汪筱林.克拉通边缘盆地碳酸盐层序地层学分析—以uhuabei板块东部早古生代沉积为例[J].长春地质学院学报,1993,23(4)
[33]陆彦邦等.安徽两淮地区奥陶纪层序地层海平面变化[J].安徽地质,1993,3(3)
[34]冯增昭,王英华,刘焕杰.中国沉积学[M].北京:石油工业出版社,1994年:1-896
[35]关士聪等.中国海陆变迁海域沉积相与油气[M].北京:科学出版社,1984.1-104
[36]王鸿祯.中国古地理图集[M].北京:地图出版社,1985:41-130
[37]刘宝珺曾允孚.岩相古地理基础与工作方法[M].地质出版社,1985年
[38]刘焕杰著.准格尔煤田含煤建造岩相古地理学研究[M].出版:地质出版社, 1991
[39]唐开疆.华北陆台晚古生代岩相古地理[J].沉积学报,1989,7(4):97-104
[40]盛吉虎、张恩惠.河南省早二叠世早期岩相古地理及聚煤作用研究[J].河南地质,1997,15(3):186-191
[41]许效松.古地理研究的前景与挑战[J].古地理学报,1999,1(4):1-11
[42]魏怀习.华北晚古生代煤系古地理演化[J].中国煤田地质,2001,13(4):14-15
[43]徐振永,王延斌等.沁水盆地晚古生代煤系层序地层及岩相古地理研究[J].煤田地质与勘探,2007,35(4):5-8
[44]蒋维红,董春梅等.岩相古地理研究现状及发展趋势[J].断块油气田,2007,14(3):1-3
[45]吴根耀.造山带古地理学——重建区域构造古地理的若干思考[J].古地理学报,2007,9(6):635-650
[46]朱如凯、许怀先.中国北方地区二叠纪岩相古地理[J].古地理学报,2007,9(2):133-142
[47]阎存凤、袁剑英、赵应成.被祁连东部石炭纪岩相古地理[J].沉积学报,2008,26(2):193-201
[48]陈晋镳、武铁山.全国地层多重划分对比研究10——华北区区域地层[M].武汉:中国地质大学出版社,1997,65-81
[49]河南省地质矿产局.河南省区域地质志[M].北京:地质出版社,1989,205-215
[50]张海清、李进化等.河南省地层古生物研究第四分册——晚古生代(华北型)[M].郑州:黄河水利出版社,2008,17-26
[51]辛仁臣,李桂范,王平在.河南永城地区上古生界沉积体系及其演化规律分析[J].黑龙江矿业学院学报,1996,6(12):11—18
[52]李文前,刘国志.豫东地区晚古生界聚煤规律研究[J].中国矿业,2008,17(6):58-61
[53]刘光华.河南禹县上石盒子组第六、七煤段沉积环境与聚煤特点[J].地质论评,1984,30(5)446-456
[54]江西煤田地质勘探公司、龚绍礼.河南禹县早二叠世晚期浅水三角洲沉积和聚煤环境[J].煤田地质,1986,1-8
[55]尹国勋.禹县煤田二叠系三煤段沉积环境与三9煤找煤方向[J].焦作矿业学院学报,1987,2:45-55
[56]翟玉琛.豫西登封煤田暴雨山井田上石盒子组第四含煤段沉积环境及聚煤特征[J].湘潭矿业学院学报,1991,6(2):112-116
[57]王果寿、裴振洪等.豫西地区中、下二叠统沉积特征[J].天然气工业,2003,23(6):24-29
[58]孙国忠、李永高.禹州市白庙矿含煤地层沉积环境及聚煤特征分析[J].中国煤炭地质,2008,20(增刊):19-21
[59]杨起.《河南禹县晚古生代煤系沉积环境与聚煤特征》[M].北京:地质出版社,1987,1-234
[60]郭熙年、唐仲林、李万程等.《河南省晚古生代聚煤规律》[M].武汉:中国地质大学出版社,1991年,1-321
[61]席文祥、裴放.《河南省岩石地层》[M].武汉:中国地质大学出版社,1997,116-148
[62]杨关秀.《中国豫西二叠纪华夏植物群——禹州植物群》[M].北京:地质出版社,2006,1-375
[63]王仁农.豫东二叠系[J].中国矿业学院学报,1982,2:50-60
[64]张士,焦清典.Lingula化石在嵩箕地区上石盒子组大量出现及其意义[J].煤田地质与勘探,1991,1:17-19
[65]王果寿、裴振洪等.豫西地区中、下二叠统沉积特征[J].天然气工业,2003,23(6):24-27
[66]魏魁生,徐怀大,叶淑蓉等.松辽盆地白垩系高分辨率层序地层格架[J].石油与天然气地质,1997,18(1):4-7
[67]吴朝容,郑荣才.辽河油田西部洼陷抄河街组高分辨率层序地层学特征[J].成都理工学院学报,1999,26(4):375-381
[68]邓宏文,王洪亮.李小孟.高分辨率层序地层对比在河流相中的应用[J].石油与天然气地质,1997,18(2):90-95
[69]王洪亮,邓宏文.地层基准面原理在胡相储层预测中的应用[J].石油与天然气地质,1997.18(2):96～102
[70]邓宏文,徐长费,王洪亮.陆东凹陷上侏罗统层序地层与生储盖组台[J].石油与天然气地质,1998,19(4):275-279
[71]郑荣才,吴朝容.西部凹陷辣层抄河街组生储盖组台的层序分析[J].成都理工学院学报,1999,26(4):348-356
[72]郑荣才,尹世民,彭军.基准面旋回结构与叠加样式的沉积动力学分析[J].沉积学报,2000,18(3):369-375
[73]郑荣才.四川盆地下侏罗统大安寨段高分辨率层序地层学特征[J].沉积学报,1998,16(2):42-49
[74]吴朝容,郑荣才.辽河油田西部洼陷抄河街组高分辨率层序地层学特征[J].成都理工学院学报,1999,26(4):375-381
[75]柳梅青,陈亦军,郑荣才.川西新场气田蓬莱镇组陆相地层高分辨率层序地层学研究[J].沉积学报,2000,18(1):50-56
[76]林万智等.中超板块晚古生代的古地磁特征[J].物探与化探,1984,5
[77]刘育燕,杨巍然,森永速男等.华北陆块、秦岭地块和扬子陆块构造演化的古地磁证据[J].地质科技情报,1993,12(4)
© 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 |