河南省西部中二叠统山西组聚煤环境及沉积演化特征
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摘要
本论文采用沉积学原理与岩相古地理研究的编图方法,通过野外地质剖面的实地测量与岩性描述,并结合收集到的野外露头、钻孔岩芯和测井等相关资料,分析了河南省西部地区山西组各种沉积相的沉积特征及沉积序列、聚煤环境和沉积演化特征,编制了研究区山西组地层综合柱状图、相柱状图、地层等厚线图、砂泥比等值线图和岩相古地理图,在此基础上取得以下主要工作进展:(1)本次工作共绘制河南省中二叠统山西组综合柱状图6张,相柱状图7张,地层等厚线图,砂泥比等值线图,构造古地理图,岩相古地理图和聚煤环境模式图各1张; (2)经综合分析在研究区山西组划分出5种沉积相,7种亚相,6种微相和14种沉积序列类型;(3)分析了整个研究区山西组聚煤环境及沉积序列特征,论述了河南省西部地区存在的两种聚煤环境模式,即三角洲分流间湾泥炭沼泽和潮坪聚煤环境。其中潮坪聚煤环境包括低位泥炭坪和高位淡水泥炭沼泽两种聚煤环境。讨论了各聚煤环境在区域上的分布特点;(4)总结了山西组沉积时期的环境演化过程,将其划分为下二煤旋回、中二煤旋回和上二煤旋回三个较大的沉积阶段。其沉积环境经历了海湾和泻湖—潮坪—下三角洲平原—上三角洲平原四种沉积环境的演变过程。
Based on the sedimentological theory, compiled map method of lithofacies paleogeography, the field measurements and lithological description of the outcrops, and combing with the relevant geologic informations including the outcrop, drilling cores and logging data, the integrated stratigraphic column, sedimentary facies column, the stratigraphic isopach map, sand-mud ratio contour map and lithofacies palaeogeography map of the Shanxi Formation have been drawn out in this work, meanwhile, the sedimentary characteristics and depositional successions of the various sedimentary facies, coal-accumulating environment and the characteristics of sedimentary evolution have been analyzed in the study area.On this basis, this paper made great progress in the following aspects:
First, seven kinds of maps have been compiled in this work, including six pieces of integrated stratigraphic column, seven pieces of sedimentary facies column, the stratigraphic isopach map, sand-mud ratio contour map, tectonic palaeogeography map, lithofacies palaeogeography map and coal accumulating environment model of the Middle Permian Shanxi Formation, western Henan province.
Second, on the basis of comprehensive analysis, five types of sedimentary facies, 7 sub-facies, six micro-facies, and 14 kinds of sedimentary successions in the Shanxi Formation of western Henan have been divided.
Third, the coal accumulating environment and depositional sequence features in Shanxi Formation of western Henan are analyzed, and two kinds of coal accumulating environment models in the Shanxi Formation of western Henan, that is, deltaic interdistributary peat bog and tidal flat coal accumulating environments, in which latter contains low-level peat flat and high-level freshwater peat bog, are suggested. The distribution features of different coal accumulating environments in this region are also discussed.
In the end, the evolution of depositional environment during the depositional period of the Shanxi Formation are Summarized, it can be divided into three large deposit phases, including the lower cycle of the coal II unit, the middle cycle of the coal II unit and the upper cycle of the coal II unit, and experienced a development of sedimentary environments from the bay and lagoon to tidal flat, and then to Lower delta plain and Upper delta plain.
Based on the sedimentological theory, compiled map method of lithofacies paleogeography, the field measurements and lithological description of the outcrops, and combing with the relevant geologic informations including the outcrop, drilling cores and logging data, the integrated stratigraphic column, sedimentary facies column, the stratigraphic isopach map, sand-mud ratio contour map and lithofacies palaeogeography map of the Shanxi Formation have been drawn out in this work, meanwhile, the sedimentary characteristics and depositional successions of the various sedimentary facies, coal-accumulating environment and the characteristics of sedimentary evolution have been analyzed in the study area.On this basis, this paper made great progress in the following aspects:
First, seven kinds of maps have been compiled in this work, including six pieces of integrated stratigraphic column, seven pieces of sedimentary facies column, the stratigraphic isopach map, sand-mud ratio contour map, tectonic palaeogeography map, lithofacies palaeogeography map and coal accumulating environment model of the Middle Permian Shanxi Formation, western Henan province.
Second, on the basis of comprehensive analysis, five types of sedimentary facies, 7 sub-facies, six micro-facies, and 14 kinds of sedimentary successions in the Shanxi Formation of western Henan have been divided.
Third, the coal accumulating environment and depositional sequence features in Shanxi Formation of western Henan are analyzed, and two kinds of coal accumulating environment models in the Shanxi Formation of western Henan, that is, deltaic interdistributary peat bog and tidal flat coal accumulating environments, in which latter contains low-level peat flat and high-level freshwater peat bog, are suggested. The distribution features of different coal accumulating environments in this region are also discussed.
In the end, the evolution of depositional environment during the depositional period of the Shanxi Formation are Summarized, it can be divided into three large deposit phases, including the lower cycle of the coal II unit, the middle cycle of the coal II unit and the upper cycle of the coal II unit, and experienced a development of sedimentary environments from the bay and lagoon to tidal flat, and then to Lower delta plain and Upper delta plain.
引文
[1]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.
[2]陈建强,周洪瑞,王训练.沉积学及古地理学教程[M].北京:地质出版社,2004年.
[3]姜在兴主编.沉积学[M].北京:石油工业出版社,2003年.
[4]何幼斌,王文广.沉积岩与沉积相[M].北京:石油工业出版社,2007年.
[5]赵澄林.沉积学原理[M].北京:石油工业出版社,2001年.
[6]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.
[7]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.
[8] Udden J A . Geology and mineral resources of the Peoria quadrangle, Illinois[J].U.S.Geol.Surv.Bull.,1912,506:103.
[9]程昭斌,汤友谊,曹廷会等.河南登封煤田马岭山井田山西组煤、岩层对比[J].焦作矿业学院学报,1989,14(1):41-51.
[10]金世雄.河南省北方型石炭一二叠纪煤系地层划分[J].河南地质,1990,8(2):38-44.
[11]李国胜,杨锐.对陕渑煤田太原组与山西组界线划分的新认识[J].河南地质,1992,10(2):112-119.
[12]牛百礼,焦清典,张士.嵩箕地区山西组的新认识[J].河南地质,1995,13(1):29-37.
[13]裴放.河南省华北型石炭一二叠纪地层多重划分与对比[J].河南地质,1998,16(4):273-280.
[14]林又玲,吴贤涛,陈江峰等.平顶山构造复杂区煤、岩层高精度对比[J].焦作工学院学报(自然科学版),2001,20(3):180-185.
[15]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年.
[16]陈书龙,孟凡顺等.豫西登封煤田马岭山一带山西组沉积环境及二1煤层厚度变化因素分析[J].焦作矿业学院学报,1987,(1):21-31
[17]陈书龙,李凯琦,谢洪波.登封煤田中部早二叠世早期海岸线形态分析[J].焦作矿业学院学报,1995,14(6):7-12.
[18]陈书龙,刘植恒,邓寅生等.豫西登封煤田白坪一带山西组沉积相、沉积体系及成煤模式[J].焦作矿业学院学报,1991,3(24):58-67.
[19]尹国勋.禹县煤田二叠系三煤段沉积环境与三9煤找矿方向[J].焦作矿业学院学报,1987,(2):45-55.
[20]张年茂,杨起,李宝芳.豫西荥巩-新密煤田太原组、山西组的沉积环境和聚煤规律[J].现代地质,1988,2(2):226-240.
[21]苏现波,盛建海,李元建.河南山西组二1煤古泥炭沼泽的类型及演化[J].煤田地质与勘探,1993,21(2):11-17.
[22]金世雄.河南省石炭-二叠纪含煤地层含煤性[J].河南地质,1996,14(3):176-185.
[23]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.
[24]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.
[25]刘彬堂.宜洛煤田二叠系下统山西组沉积环境分析[J].西部探矿工程(WEST-CHINA EXPLORATION ENGINEERING),2006,18(4).
[26]罗锐,刘传喜,许军等.豫西陕渑煤田东部石炭二叠纪含煤岩系岩相古地理分析[J].中州煤炭,2007,(1):27-29.
[27]张海清.Emplectopteridium在禹县剖面中两次出现的时代意义[J].中国区域地质,1989,(3):243-246.
[28]张士.河南登封晚古生代含煤地层各煤组的古生物特征[J].地层学杂志,1990,14(2):140-144.
[29]姚庚云,陈书龙,刘植恒等.豫西登封煤田白坪井田“山西组”的植物化石[J].焦作矿业学院学报,1991,(4):1-15(总第25期).
[30]张士,姚庚云,姚兆奇.河南西部“山西组”含大羽羊齿植物的层位[J].地层学杂志,1991,15(3):215-220.
[31]杜慧英,王家德.河南省山西组孢粉组合特征及环境意义[J].河南地质(HENAN GEOLOGY),1994,12(3):198-203.
[32]王军,孙柏年.河南登封二叠纪煤系地层植物化石组合[J].河南地质,1996,14(4):272-276.
[33]王军,孙柏年,沈光隆.豫西—皖北地区二叠纪植物地理区系性质探讨[J].高校地质学报,1999,5(1):76-91.
[34]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年.
[35]河南省地质矿产局.河南省区域地质志[M].北京:地质出版社,1990年.
[36]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年.
[37]陈晋镳,武铁山.华北区区域地层[M].武汉:中国地质大学出版社,1997年.
[38]张旭东,张旭彤,马东.河南省济源西部山西组煤层特征及聚煤环境分析[J].煤,2009,18(4):61-64.
[39]陈书龙,刘植恒,邓寅生等.豫西登封白坪地区山西组沉积相序及煤厚控制因素研究[J].焦作矿业学院学报,1995,14(2):10-18.
[40]魏怀习.河南新郑矿区山西组沉积环境与聚煤特征[J].中国煤田地质,1989,1(2):30-35.
[41]赵群华,王可,王琳.平顶山二矿山西组沉积环境对煤层厚度的影响[J].焦作工学院学报,2003,22(3):187-189.
[42]周慧堂,王天顺.豫西陕渑煤田山西组煤层形成环境和聚煤特征[J].沉积学报,1989,7(4):121-131.
[43]张年茂,杨起,李宝芳.预西荥巩—新密煤田太原组、山西组的沉积环境和聚煤规律[J] .现代地质,1988,2(2):226-240.
[44]李宝芳,刘光华,李祯等.豫西太原组、山西组中潮道沉积的类型和特征[J].沉积学报,1988,6(2):31-42.
[45]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.
[46]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.
[47]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.
[48]陈世悦,徐凤银,刘焕杰.华北晚古生代层序地层与聚煤规律[M].山东:石油大学出版社,2000年.
[49] Weller J M.Cyclic sedimentation of the Pennsylvanian period and its significance[J].Journal of Geology,1930,38:97-135
[50] 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
[51] 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
[52] Klein GD. Estimating water depths from analysis of barrier island anddeltaic sedimentary sequences. Geology, 1974, 21: 409～412
[53]徐汉林、赵宗举、吕福亮等.南华北地区的构造演化与含油气性[J].大地构造与成矿学,2004.28(4):450-463
[54]王鸿祯等.中国及邻区构造古地理和生物古地理[M].武汉:中国地质大学出版社,1990.08
[55]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
[56]王鸿祯.中国古地理图集[M].北京:地图出版社,1985:41-130
[57]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
[58]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
[59]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
[60]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
[61]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
[62] 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.
[63] 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.
[64] 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
[65] McCabe P J.Sedimentary environment of coal and coal-bearing strata.Spec. public. In1.A ss Sediment 1984,7,P13-42
[66] Woodcock N H.Sequence stratigraphy of the Palaeozoic Welsh Basin..Journal of the Geological society,1990,Vol.147
[67] Reading H G. Sedimentary environments and facies.Oxford London.Blackwall scientific publications,I978
[68] Allen P A, Collinson J D. Lakes. In: Reading H G, ed. Sedimentary environments and facies. Oxford: Blackwell Scientific Publications,1986. 63-94
[69] WrightL D. Sediment transport and deposition at rivermouths: a synthesis. Geological Society of America Bulletin, 1977, 88: 857-868
[70] Coleman J M, Prior D B. Deltaic sand bodies. AAPG Short CourseNote Series 1980, 15: 171
[71] 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
[72] Bridge J S.Large scale facies sequences in alluvial overbank environments.J. Sediment-Petrol.1984,54,583-588
[73] Galloway, W. E.,Hobday, D. K., 1983, Terrigenous Clastic Depositional Systems. Springer-Verlag, N. Y. Inc.
[2]陈建强,周洪瑞,王训练.沉积学及古地理学教程[M].北京:地质出版社,2004年.
[3]姜在兴主编.沉积学[M].北京:石油工业出版社,2003年.
[4]何幼斌,王文广.沉积岩与沉积相[M].北京:石油工业出版社,2007年.
[5]赵澄林.沉积学原理[M].北京:石油工业出版社,2001年.
[6]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.
[7]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.
[8] Udden J A . Geology and mineral resources of the Peoria quadrangle, Illinois[J].U.S.Geol.Surv.Bull.,1912,506:103.
[9]程昭斌,汤友谊,曹廷会等.河南登封煤田马岭山井田山西组煤、岩层对比[J].焦作矿业学院学报,1989,14(1):41-51.
[10]金世雄.河南省北方型石炭一二叠纪煤系地层划分[J].河南地质,1990,8(2):38-44.
[11]李国胜,杨锐.对陕渑煤田太原组与山西组界线划分的新认识[J].河南地质,1992,10(2):112-119.
[12]牛百礼,焦清典,张士.嵩箕地区山西组的新认识[J].河南地质,1995,13(1):29-37.
[13]裴放.河南省华北型石炭一二叠纪地层多重划分与对比[J].河南地质,1998,16(4):273-280.
[14]林又玲,吴贤涛,陈江峰等.平顶山构造复杂区煤、岩层高精度对比[J].焦作工学院学报(自然科学版),2001,20(3):180-185.
[15]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年.
[16]陈书龙,孟凡顺等.豫西登封煤田马岭山一带山西组沉积环境及二1煤层厚度变化因素分析[J].焦作矿业学院学报,1987,(1):21-31
[17]陈书龙,李凯琦,谢洪波.登封煤田中部早二叠世早期海岸线形态分析[J].焦作矿业学院学报,1995,14(6):7-12.
[18]陈书龙,刘植恒,邓寅生等.豫西登封煤田白坪一带山西组沉积相、沉积体系及成煤模式[J].焦作矿业学院学报,1991,3(24):58-67.
[19]尹国勋.禹县煤田二叠系三煤段沉积环境与三9煤找矿方向[J].焦作矿业学院学报,1987,(2):45-55.
[20]张年茂,杨起,李宝芳.豫西荥巩-新密煤田太原组、山西组的沉积环境和聚煤规律[J].现代地质,1988,2(2):226-240.
[21]苏现波,盛建海,李元建.河南山西组二1煤古泥炭沼泽的类型及演化[J].煤田地质与勘探,1993,21(2):11-17.
[22]金世雄.河南省石炭-二叠纪含煤地层含煤性[J].河南地质,1996,14(3):176-185.
[23]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.
[24]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.
[25]刘彬堂.宜洛煤田二叠系下统山西组沉积环境分析[J].西部探矿工程(WEST-CHINA EXPLORATION ENGINEERING),2006,18(4).
[26]罗锐,刘传喜,许军等.豫西陕渑煤田东部石炭二叠纪含煤岩系岩相古地理分析[J].中州煤炭,2007,(1):27-29.
[27]张海清.Emplectopteridium在禹县剖面中两次出现的时代意义[J].中国区域地质,1989,(3):243-246.
[28]张士.河南登封晚古生代含煤地层各煤组的古生物特征[J].地层学杂志,1990,14(2):140-144.
[29]姚庚云,陈书龙,刘植恒等.豫西登封煤田白坪井田“山西组”的植物化石[J].焦作矿业学院学报,1991,(4):1-15(总第25期).
[30]张士,姚庚云,姚兆奇.河南西部“山西组”含大羽羊齿植物的层位[J].地层学杂志,1991,15(3):215-220.
[31]杜慧英,王家德.河南省山西组孢粉组合特征及环境意义[J].河南地质(HENAN GEOLOGY),1994,12(3):198-203.
[32]王军,孙柏年.河南登封二叠纪煤系地层植物化石组合[J].河南地质,1996,14(4):272-276.
[33]王军,孙柏年,沈光隆.豫西—皖北地区二叠纪植物地理区系性质探讨[J].高校地质学报,1999,5(1):76-91.
[34]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年.
[35]河南省地质矿产局.河南省区域地质志[M].北京:地质出版社,1990年.
[36]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年.
[37]陈晋镳,武铁山.华北区区域地层[M].武汉:中国地质大学出版社,1997年.
[38]张旭东,张旭彤,马东.河南省济源西部山西组煤层特征及聚煤环境分析[J].煤,2009,18(4):61-64.
[39]陈书龙,刘植恒,邓寅生等.豫西登封白坪地区山西组沉积相序及煤厚控制因素研究[J].焦作矿业学院学报,1995,14(2):10-18.
[40]魏怀习.河南新郑矿区山西组沉积环境与聚煤特征[J].中国煤田地质,1989,1(2):30-35.
[41]赵群华,王可,王琳.平顶山二矿山西组沉积环境对煤层厚度的影响[J].焦作工学院学报,2003,22(3):187-189.
[42]周慧堂,王天顺.豫西陕渑煤田山西组煤层形成环境和聚煤特征[J].沉积学报,1989,7(4):121-131.
[43]张年茂,杨起,李宝芳.预西荥巩—新密煤田太原组、山西组的沉积环境和聚煤规律[J] .现代地质,1988,2(2):226-240.
[44]李宝芳,刘光华,李祯等.豫西太原组、山西组中潮道沉积的类型和特征[J].沉积学报,1988,6(2):31-42.
[45]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.
[46]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.
[47]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.
[48]陈世悦,徐凤银,刘焕杰.华北晚古生代层序地层与聚煤规律[M].山东:石油大学出版社,2000年.
[49] Weller J M.Cyclic sedimentation of the Pennsylvanian period and its significance[J].Journal of Geology,1930,38:97-135
[50] 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
[51] 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
[52] Klein GD. Estimating water depths from analysis of barrier island anddeltaic sedimentary sequences. Geology, 1974, 21: 409～412
[53]徐汉林、赵宗举、吕福亮等.南华北地区的构造演化与含油气性[J].大地构造与成矿学,2004.28(4):450-463
[54]王鸿祯等.中国及邻区构造古地理和生物古地理[M].武汉:中国地质大学出版社,1990.08
[55]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
[56]王鸿祯.中国古地理图集[M].北京:地图出版社,1985:41-130
[57]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
[58]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
[59]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
[60]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
[61]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
[62] 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.
[63] 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.
[64] 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
[65] McCabe P J.Sedimentary environment of coal and coal-bearing strata.Spec. public. In1.A ss Sediment 1984,7,P13-42
[66] Woodcock N H.Sequence stratigraphy of the Palaeozoic Welsh Basin..Journal of the Geological society,1990,Vol.147
[67] Reading H G. Sedimentary environments and facies.Oxford London.Blackwall scientific publications,I978
[68] Allen P A, Collinson J D. Lakes. In: Reading H G, ed. Sedimentary environments and facies. Oxford: Blackwell Scientific Publications,1986. 63-94
[69] WrightL D. Sediment transport and deposition at rivermouths: a synthesis. Geological Society of America Bulletin, 1977, 88: 857-868
[70] Coleman J M, Prior D B. Deltaic sand bodies. AAPG Short CourseNote Series 1980, 15: 171
[71] 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
[72] Bridge J S.Large scale facies sequences in alluvial overbank environments.J. Sediment-Petrol.1984,54,583-588
[73] Galloway, W. E.,Hobday, D. K., 1983, Terrigenous Clastic Depositional Systems. Springer-Verlag, N. Y. Inc.
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