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OALib Journal期刊
ISSN: 2333-9721
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山东埠西黄土剖面沉积特征及古气候环境意义
DOI: 10.11821/dlxb201411011, PP. 1707-1717
Keywords: 山东埠西,黄土,磁化率,光释光,粒度
Abstract:
对山东济南章丘埠西黄土剖面进行了系统的野外调查,并对山东章丘埠西黄土剖面进行了粒度、磁化率以及光释光测年等指标研究分析,结果表明①根据粒度测量数据和粒度参数变化特征,并运用萨胡判别公式对其沉积环境进行判别,可知山东埠西剖面黄土沉积主要为风成沉积。通过粒级—标准偏差方法提取的环境敏感粒级分别为7.08~8.91μm和39.81~50.12μm;②磁化率变化与不同粒级百分含量的变化之间具有明显的相关性,其中低频磁化率变化范围为32.38×10-8~138.46×10-8m3kg-1,高频磁化率在30.62×10-8~123.31×10-8m3kg-1之间变化,其变化特征一定程度上反映了埠西黄土剖面形成时的古气候环境信息;③结合光释光年代的测量数据与前人的研究成果,可将该黄土剖面划分为3个黄土层和3个古土壤层,该剖面记录了末次冰期以来该区域古气候环境的变化历史过程。
| [1] | DingXigui,YeSiyuan,GongShaojunetal.Analysisonenvironmentallysensitivegrain-sizepopulationandsedimentaryenvironmentofZK1drillingcoreinYellowRiverDelta.GlobalGeology,2010,29(4):575-581.[丁喜桂,叶思源,宫少军等.黄河三角洲ZK1孔岩心环境敏感粒度组分及沉积环境分析.世界地质,2010,29(4):575-581.]
|
| [2] | ChengduGeologicalInstitute.SedimentaryParticleSizeAnalysisandItsApplication.Beijing:GeologicalPublishingHouse,1976:31-127.[成都地质学院陕北队.沉积岩(物)粒径分析及其应用.北京:地质出版社,1976:31-127.]
|
| [3] | LongHao,WangNai-ang,LiYuetal.ParticlesizecharacteristicsofdepositsfromPJHZsectioninnorthernedgeofMuUsDesertandtheirenvironmentalsignificance.JournalofDesertResearch,2007,27(2):187-193.[隆浩,王乃昂,李育等.毛乌素沙地北缘泊江海子剖面粒度特征及环境意义.中国沙漠,2007,27(2):187-193.]
|
| [4] | LiJiyan,DongZhibao,LiEnjuetal.Grain-sizecharacteristicsofthedepositsfromYardanglandformsintheCharhanSaltLakearea.JournalofDesertResearch,2012,32(5):1187-1192.[李继彦,董治宝,李恩菊等.察尔汗盐湖雅丹地貌沉积物粒度特征研究.中国沙漠,2012,32(5):1187-1192.]
|
| [5] | SunDonghuai,AnZhisheng,SuRuixiaetal.Mathematicalapproachtosedimentarycomponentpartitioningofpolymodalsedimentsanditsapplications.ProgressinNaturalScience,2001,11(3):269-276.[孙东怀,安芷生,苏瑞侠等.古环境中沉积物粒度组分分离的数学方法及其应用.自然科学进展,2001,11(3):269-276.]
|
| [6] | SunYoubin,GaoShu,LiJun.Preliminaryanalysisofgrain-sizepopulationswithenvironmentallysensitiveterrigenouscomponentsinmarginalseasetting.ChineseScienceBulletin,2003,48(1):83-86.[孙有斌,高抒,李军.边缘海陆源物质中环境敏感粒度组分的初步分析.科学通报,2003,48(1):83-86.]
|
| [7] | ChenQiao,LiuDongyan,ChenYijunetal.Comparativeanalysisofgrade-standarddeviationmethodandfactorsanalysismethodforenvironmentalsensitivefactoranalysis.EarthandEnvironment,2013,41(3):319-325.[陈桥,刘东艳,陈颖军等.粒级—标准偏差法和主成分因子分析法在粒度敏感因子提取中的对比.地球与环境,2013,41(3):319-325.]
|
| [8] | XuShujian,PanBaotian,GaoHongshanetal.Analysisofgrain-sizepopulationswithenvironmentallysensitivecomponentsofloessduringthelastinterglacial-glacialcycleandtheirimplications.ActaPedologicaSinica,2006,43(2):183-189.[徐树建,潘保田,高红山等.末次间冰期—冰期旋回黄土环境敏感粒度组分的提取及意义.土壤学报,2006,43(2):183-189.]
|
| [9] | LinBingyao.IntroductiontoQuantitativeGeography.Beijing:HigherEducationPress,1985:29-33.[林炳耀.计量地理学概论.北京:高等教育出版社,1985:29-33.]
|
| [10] | LuHuayu,AnZhisheng.Grain-sizecompositionofLuochuanloessandpaleoclimateimplication.ChineseScienceBulletin,1997,42(1):66-69.[鹿化煜,安芷生.洛川黄土粒度组成的古气候意义.科学通报,1997,42(1):66-69.]
|
| [11] | ThompsonR,OldfieldF.EnvironmentalMagnetism.Beijing:GeologicalPublishingHouse,1995:22-23.[汤普森R,奥尔德菲尔德F.环境磁学.北京:地质出版社,1995:22-23.]
|
| [12] | LiuDongsheng.LoessandEnvironment.Beijing:SciencePress,1985:191-207.[刘东生.黄土与环境.北京:科学出版社,1985:191-207.]
|
| [13] | AnZhisheng,LiuTungsheng,LuYanchouetal.Thelong-termpaleomonsoonvariationrecordedbytheloess-paleosolsequenceincentralChina.QuaternaryInternational,1990,7/8:91-95.
|
| [14] | ChenMingyang.TheevolutionofChineseaeoliandepositsandglobalaridification.QuaternarySciences,1991,(4):361-372.[陈明扬.中国风尘堆积与全球干旱化.第四纪研究,1991,(4):361-372.]
|
| [15] | AnZS,KutzbachJE,PrellWLetal.EvolutionofAsianmonsoonsandphasedupliftoftheHimalaya-TibetanPlateausinceLateMiocenetimes.Nature,2001,411(6833):62-66.
|
| [16] | GuoZT,RuddimanWF,HaoQZetal.OnsetofAsiandesertificationby22MyragoinferredfromloessdepositsinChina.Nature,2002,416(6877):159-163.
|
| [17] | SunDonghuai,LuHuayu.Grain-sizeanddustaccumulationrateofLateCenozoicaeoliandepositsandtheinferredatmosphericcirculationevolutions.QuaternarySciences,2007,27(2):251-262.[孙东怀,鹿化煜.晚新生代黄土高原风尘序列的粒度和沉积速率与中国北方大气环流演变.第四纪研究,2007,27(2):251-262.]
|
| [18] | WenQizhongetal.GeochemistryofChineseLoess.BeijingSciencePress,1989:1-285.[文启忠等著.中国黄土地球化学.北京:科学出版社,1989:1-285.]
|
| [19] | YuHongjun.AnewexplorationontheoriginofloessintheshelfareaoftheeasternChinaseas.QuaternaryScience,1999,7(4):366-372.[于洪军.中国东部陆架黄土成因的新探索.第四纪研究,1999,7(4):366-372.]
|
| [20] | CaoJiaxin,LiPeiying,ShiNing.TheloessofMiaodaoIslandsofShandong.ScienceinChina:SeriesB,1987,17(10):1116-1123.[曹家欣,李培英,石宁.山东庙岛群岛的黄土.中国科学:B辑,1987(10):1116-1123.]
|
| [21] | LiuLejun,LiPeiying,WangYongji.Thegrain-sizepropertiesandgenesisofloessincentralShandongProvince.MarineGeology&QuaternaryGeology,2000,20(1):81-86.[刘乐军,李培英,王永吉.鲁中黄土粒度特征及其成因探讨.海洋地质与第四纪地质,2000,20(1):81-86.]
|
| [22] | ZhangZulu,XinLiangjie,NieXiaohong.AsummaryofloessialresearchesinShandong.ScientiaGeographicaSinica,2004,24(6):746-752.[张祖陆,辛良杰,聂晓红.山东地区黄土研究综述.地理科学,2004,24(6):746-752.]
|
| [23] | XuShujian.GrainsizecharacteristicsanditsindicationsofloessinMiaodaoIslands,ShandongProvince.MarineSciences,2008,32(12):60-63.[徐树建.山东庙岛群岛黄土的粒度特征及其环境意义.海洋科学,2008,32(12):60-63.]
|
| [24] | DingZhongli,RenJianzhang,LiuDongshengetal.Themechanismsofthemillennium-scaleirregularchangeofthelatePleistocenemonsoon-desertsystem.ScienceinChina:SeriesD,1996,26(5):386-391.[丁仲礼,任剑璋,刘东生,等.晚更新世季风—沙漠系统千年尺度不规则变化及其机制问题.中国科学:D辑,1996,26(5):386-391.]
|
| [25] | LuHuayu,AnZhisheng.Paleoclimaticsignificanceofgrainsizeofloess-palaeosoldepositinChineseLoessPlateau.ScienceinChina:SeriesD,1998,28(3):278-283.[鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义.中国科学:D辑,1998,28(3):278-283.]
|
| [26] | AnZhisheng,PorterS,KuklaGetal.EvidencefrommagneticsusceptibilityofmonsoonevolutionontheLoessPlateausincethelast130000years.ChineseScienceBulletin,1990,35(7):529-532.[安芷生,PorterS,KuklaG等.最近13万年黄土高原季风变迁的磁化率证据.科学通报,1990,35(7):529-532.]
|
| [27] | LiuXiuming,LiuTungsheng,HellerFetal.Frequencydevelopmentsusceptibilityofloess.QuaternarySciences,1990,10(1):42-50.[刘秀铭,刘东生,HellerF等.黄土频率磁化率与古气候冷暖变换.第四纪研究,1990,10(1):42-50.]
|
| [28] | SunDonghuai,ChenMingyang,ShowJohnetal.MagnetostratigraphyandpaleoclimaterecordsoflateCenozoiceoliansequenceintheLoessPlateauofChina.ScienceinChina:SeriesD,1998,28(1):79-84.[孙东怀,陈明扬,ShawJohn等.晚新生代黄土高原风尘堆积序列的磁性地层年代与古气候记录.中国科学:D辑,1998,28(1):79-84.]
|
| [29] | LiuXiuming,LiuDongsheng,HellerFriedrichetal.ResearchofmagneticsusceptibilityofChineseloessandQuaternarypaleoclimate.ScientiaGeologicaSinica,1992,(Suppl.):279-285.[刘秀铭,刘东生,HellerFriedrich等.中国黄土磁化率与第四纪古气候研究.地质科学,1992,(Suppl.):279-285.]
|
| [30] | ZhangJiafu,MoDowen,XiaZhengkaietal.OpticaldatingofsedimentsfromChinaanditsimplicationfordepositionalprocesses.QuaternarySciences,2009,29(1):23-33.[张家富,莫多闻,夏正楷等.沉积物的光释光测年和对沉积过程的指示意义.第四纪研究,2009,29(1):23-33.]
|
| [31] | TimarA,VandenbergheD,PanaiotuECetal.OpticaldatingofRomanianloessusingfine-grainedquartz.QuaternaryGeochronology,2010,5(2/3):143-148.
|
| [32] | XinLiangjie.CharacteristicsofthecompositionoftheZhangxialoessanditsorigin.GeologyinChina,2005,32(1):55-61.[辛良杰.张夏黄土组成特征及其成因分析.中国地质,2005,32(1):55-61.]
|
| [33] | WangQiuliang,LiChangan,XieYuanyunetal.Grain-sizecharacteristicsofsedimentsintheJianglingsectionandtheirpaleoclimaticsignificance.GeologyinChina,2006,33(6):1406-1410.[王秋良,李长安,谢远云等.江陵剖面沉积物的粒度特征及其古气候意义.中国地质,2006,33(6):1406-1410.]
|
| [34] | LuHuayu,AnZhisheng.Comparisonofgrain-sizedistributionofredclayandloess-paleosoldepositsinChineseLoessPlateau.ActaSedimentologicaSinica,1999,17(2):226-232.[鹿化煜,安芷生.黄土高原红黏土与黄土古土壤粒度特征对比:红黏土风成成因的新证据.沉积学报,1999,17(2):226-232.]
|
| [35] | LiuDongyan,LiWeiran,PengShashaetal.CurrentapplicationofgrainsizeanalysisinChineseloesspaleoclimaticstudy.PeriodicalofOceanUniversityofChina,2010,40(2):79-84.[刘冬雁,李巍然,彭莎莎等.粒度分析在中国第四纪黄土古气候研究中的应用现状.中国海洋大学学报:自然科学版,2010,40(2):79-84.]
|
| [36] | WangH,LiuH,CuiHetal.TerminalPleistocene/HolocenepalaeoenvironmentalchangesrevealedbymineralmagnetismmeasurementsoflakesedimentsforDaliNorarea,southeasternlnnerMongoliaPlateau,China.Palaeogeography,Palaeoclimatology,Palaeoecology,2001,170:115-132.
|
| [37] | ChenHongyun,SunYoubin.StudyonprovenanceofeoliandustdepositsontheChineseLoessPlateau:Retrospectsandprospects.QuaternarySciences,2008,28(5):892-900.[陈洪云,孙有斌.黄土高原风尘沉积的物质来源研究:回顾与展望.第四纪研究,2008,28(5):892-900.]
|
| [38] | AnZhisheng,KuklaG,LiuTungsheng.LoessstratigraphyinLuochuanofChina.QuaternarySciences,1989,(2):157-168.[安芷生,KuklaG,刘东生.洛川黄土地层学.第四纪研究,1989,(2):155-168.]
|
| [39] | XuShujian,WangTao.OpticallystimulatedluminescencedatingandsedimentarycharacteristicsofloesssectionatPenglaiinShandongProvince.JournalofDesertResearch,2011,31(2):295-301.[徐树建,王涛.蓬莱黄土剖面光释光年代学及其沉积特征研究.中国沙漠,2011,31(2):295-301.]
|
| [40] | FuJie,LiYonghua,ZhangHuaetal.CharacteristicofmagneticsusceptibilityanditsprimarilyinterpretationoflateCenozoicsedimentsinLiaodongPeninsula.JournalofAridLandResourcesandEnvironment,2014,28(3):135-141.[伏捷,李永化,张华等.辽东半岛晚新生代沉积物磁化率特征及初步解释.干旱区资源与环境,2014,28(3):135-141.]
|
| [41] | ChenJie,LuYanchou,WeiLanyingetal.OpticallystimulatedluminescencedatingofQuaternarysediments:Acomparisonusingdifferentequivalentdosedeterminationmethods.Geochimica,1990,28(5):443-452.[陈杰,卢演俦,魏兰英等.第四纪沉积物光释光测年中等效剂量测定方法的对比研究.地球化学,1999,28(5):443-452.]
|
| [42] | MaYugai,HuangChunchang,ZhouYalietal.OSLDatingofthepalaeofloodeventintheShangjiahereachintheupperHanjiangRivervalley.ActaSedimentologicaSinica,2014,32(2):306-313.[马玉改,黄春长,周亚利等.汉江上游尚家河段全新世古洪水事件光释光测年研究.沉积学报,2014,32(2):306-313.]
|
| [43] | ZhangWei,YuYang,LiuBeibeietal.StudyontheloesslayerinthesouthofLiaoningProvinceusingtheopticallystimulatedluminescence.EarthandEnvironment,2013,41(2):117-125.[张威,于洋,刘蓓蓓等.辽南黄土光释光年代地层探讨.地球与环境,2013,41(2):117-125.]
|
| [44] | ThomasS,GrzegorzA,AnnaFBetal.AnabruptshiftindustsourceontheChineseLoessPlateaurevealedthroughhighsamplingresolutionOSLdating.QuaternaryScienceReviews,2013,82(15):121-132.
|
| [45] | LaiZhongping,OuXianjiao.Basicproceduresofopticallystimulatedluminescence(OSL)dating.ProgressinGeography,2013,32(5):683-693.[赖忠平,欧先交.光释光测年基本流程.地理科学进展,2013,32(5):683-693.]
|
| [46] | LaiZhongping,ZhangWeiguo,ChenXietal.OSLchronologyofloessdepositsinEastChinaanditsimplicationsforEastAsianmonsoonhistory.QuaternaryGeochronology,2010,5(2/3):154-158.
|
| [47] | WintleAG,MurrayAS.Areviewofquartzopticallystimulatedluminescenceandcharacteristicsandtheirrelevanceinsingle-aliquotregenerationdatingprotocols.RadiationMeasurements,2006,41(4):369-391.
|
| [48] | MurrayAS,WintleAG.Luminescencedatingofquartzusinganimprovedsingle-aliquotregenerative-doseprotocol.RadiationMeasurements,2000,32(1):57-93.
|
| [49] | HuFangen,LiZhizhong,JinJianhuietal.CoastalenvironmentevolutionrecordfromAnshancoastalaeoliansandofJinjiang,FujianProvince,basedontheOSLdating.ActaGeographicaSinica,2013,68(3):343-356.[胡凡根,李志忠,靳建辉等.基于释光测年的福建晋江海岸沙丘粒度记录的风沙活动.地理学报,2013,68(3):343-356.]
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