全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

岱海湖泊沉积岩芯高分辨率磁性测量——U型槽与常规方法之比较

, PP. 983-988

Keywords: 岱海,U型槽,磁化率,ARM,湖泊沉积物

Full-Text   Cite this paper   Add to My Lib

Abstract:

对岱海西南部湖滨地区(40°32.127′N,112°37.802′E)钻取的一根长79.16m的高取芯率(98.8%)沉积岩芯(DH06A)进行了高分辨率的湖泊沉积物磁学性质测量。对U型槽法和常规散样方法得到的磁化率和非磁滞剩余磁化强度测量结果进行了系统的比较。

References

[1]  13 B ark er P A,L engM J,G asse F et al.C entury to m il lenn ial scaleclmi at ic variab ility in Lake M alaw i revealed by isotope records.Earth and P laneta ry Sc ience L etters,2007(in press)
[2]  14 Y an ch eva G,N ow aczyk N R,M ingram J e t a .lIn flu ence of thein tertrop ical convergence zone on th e E ast A sian m on soon.N a tu re,
[3]  20 07 ,445:74~77
[4]  15 J i J F,Shen J,Balsam W et a l.A sian m onsoon oscillations in thenortheastern Q ingha i T ibet P lateau sin ce the late glacia l asin terpreted from vis ib le reflectance of Q ingha i Lake sed im en ts.Earth and P laneta ry Sc ience L etters,2005,233(1~2):61~70
[5]  16 Peng Y J,X iao J L,N akam ura T et a .lH olocen e vegetationvariation in th e D aiha i Lake reg ion of N orth central Ch in a:A directind ication of the A s ian m onsoon clim at ic history.Q ua ternary S cien ceR ev iew s,2004,23:1669~1679
[6]  17 陈发虎,吴薇,朱艳等.阿拉善高原中全新世干旱事件的湖泊记录研究.科学通报,2004,49(1):1~9Chen Fahu,W u W ei, H olm es J A et a .lA m id H o locene droughtin terval as eviden ced by lak e des iccation in th e A lashan Plateau,InnerM ongol ia,Ch ina.C hinese S cience B ul le tin,2003,48(14):
[7]  14 01~1410
[8]  18 胡守云,邓成龙,A ppel E等.湖泊沉积物磁学性质的环境意义.科学通报,2001,46(17):1491~1494H u Shouyun,D eng Chenglong,A ppel E et a l.Environm en talm agnetic stud ies of lacus trine sed im ents.Ch in ese Science B ul le tin,2002 ,47(7):613~616
[9]  19 刘嘉麒,N egendank J F W,王文远等.中国玛珥湖的时空分布与地质特征.第四纪研究,2000,20(1):78~86L iu J iaqi, N egendank J F W,W angW enyuan et al.The d istribu tionand geolog ical characterist ics of m aar lakes in Ch in a.Q ua ternaryS ciences,2000,20(1):78~86
[10]  20 刘强,游海涛,刘嘉麒.湖泊沉积物年纹层的研究方法及其意义.第四纪研究,2004,24(6):683~694L iu Q iang,Y ou H a itao,Liu J iaqi. M ethodology of studying onvarved lake sed im ents and its sign if icance.Qua ternary Sciences,2004 ,24(6):683~694
[11]  21 薛滨,于革,王苏民.中国不同区域30000 aB P.以来湖泊水量变化特征.第四纪研究,2001,21(6):567Xu e B in,Y u G e,W ang Sum in.The changing ch aracteristics of lak ew ater volum e in Ch in a?s d ifferent regions sin ce 30000aB P.Q uaternary S ciences,2001,21(6):567
[12]  22 肖海丰,沈吉,肖霞云.云南鹤庆钻孔揭示的西南季风轨道尺度演化.第四纪研究,2006,26(2):274~282X iao H aifeng,Shen J,i X iao X iayun.The orb ital scale evo lut ion ofth e southw est m on soon reflected by the H eq ing core in Y unn anProvince.Q ua ternary S ciences,2006,26(2):274~282
[13]  23 V erosub K L.Faster is b ette.rSc ience,1998,281:1297~1298
[14]  24 孙千里,周杰,沈吉等.北方环境敏感带岱海湖泊沉积所记录的全新世中期环境特征.中国科学(D辑),2006,36(9):
[15]  83 8~849Sun Q ian li, Zhou Jie,Shen Ji e t a l.Environm en tal characteristics ofM id H olocen e recorded by lacu strine sed im en ts from Lake D aiha,inorth env ironm en t sens it ive zon e,Ch ina.S cience in C hina(S eriesD),2006,49(9):968~981
[16]  25 王苏民,余源盛,吴瑞金等.岱海湖泊环境与气候变化.合肥:中国科学技术大学出版社,1990.155~183W ang Sum in,Y u Y uansheng,W u R u ijin et al.The D aihai Lak e:Environm en t E volut ion and C l mi ate Changes.H efei: Ch ineseS cience and Techn ology U n iversity P ress,1990 155~183
[17]  26 吴瑞金.湖泊沉积物的磁化率、频率磁化率及其古气候意义以青海湖、岱海近代沉积为例.湖泊科学,1993,5(2):
[18]  12 8~135W u R u ijin.M agnetic suscept ib ility()and frequency depend entsu scept ib ility(fd)of lake sedmi en ts and their paleoclmi aticmi p lication The case of recent sed mi en ts of Q inghai Lak e andD aihai Lake.Journa l of Lake S cien ce s,1993,5(2):128~135
[19]  27 张振克,吴瑞金,王苏民.岱海湖泊沉积物频率磁化率对历史时期环境变化的反映.地理研究,1998,17(3):297~302Zh ang Zhenk e,W u R u ijin,W ang Sum in.Imp licat ion of m agneticfrequen cy d ependen t suscep tib il ity on env ironm ental variat ion fromlacu strine sed im en t in D aih ai Lake.G eographical R esearch,1998,17 (3):297~302
[20]  28 Li X iaoqiang,Zhou Jie,Sh en Ji et al.V egetation h istory andclmi atic variat ion s du ring th e last 14kaB.P.in ferred from a pollenrecord at D aihai Lake,N orth cen tral C hina.R eview of P alaeobotanyand Pa lynology,2004,132(3~4):195~205
[21]  29 Peng Y J,X iao J L,N akam ura T e t al.H olocene E ast A s ianm onsoon al precip itat ion pattern revealed by grain size d istribu tion ofcore sed im ents of D a ihai Lake in Inn er M ongol ia of N orth cen tralC h ina.E arth and P lan etary Science L etters,2005,233(3~4):467~479
[22]  30 金章东,王苏民,沈吉等.全新世岱海流域化学风化及其对气候事件的响应.地球化学,2004,33(1):29~36J in Zhangdong,W ang Sum in,Shen Ji et a l.W atershed ch em icalw eathering and its response to cl imate events in D aihai area du ringH olocene.G eoch im ica,2004,33(1):29~36
[23]  1陈 发虎,黄小忠,杨美临等.亚洲中部干旱区全新世气候变化的西风模式以新疆博斯腾湖记录为例.第四纪研究,2006,26(6):881~887C hen Fahu,Hu ang X iaozhong,Y ang M eilin e t al.W esterlydom inated H olocen e clim ate m odel in arid C entra l A sia C asestudy on B os ten Lake,X inj iang,Ch ina.Q u aternary S cience s,2006 ,26(6):881~887
[24]  2 孙千里,肖举乐.岱海沉积记录的季风/干旱过渡区全新世适宜期特征.第四纪研究,2006,26(5):781~790Sun Q ian l,i X iao Ju le.Ch aracteristics of the H olocene opt mium inthe m onsoon/arid tran sit ion b elt recorded by core sed mi en ts ofD aihai Lake,N orth Ch ina.Q u a ternary S cience s,2006,26(5):
[25]  78 1~790
[26]  3 朱立平,鞠建廷,王君波等.湖芯沉积物揭示的末次冰消开始时期普莫雍错湖区环境变化.第四纪研究,2006,26(5):772~780Zhu L iping,Ju J iant ing,W ang Junbo et a .lEnvironm ental changesrecorded in core sed mi ents from th e Pum oyum C o Lake of the T ibetanPlateau du ring the in it ial stage of the last deglacial period.Qu aternary S cience s,2006,26(5):772~780
[27]  4 张成君,陈发虎,尚华明等.中国西北干旱区湖泊沉积物中有机质碳同位素组成的环境意义以民勤盆地三角城古湖泊为例.第四纪研究,2004,24(1):88~94Zhang C hengjun,C hen Fahu,Shang H uam ing et a l.Thepaleoen vironm ental s ign if ican ce of organ ic carbon isotope inlacustrin e sed mi en ts in the arid Ch in a:A n exam p le fromSan jiaoch eng palaeolake in M inq in.Q ua ternary S cien ces,2004,24(1):88~94
[28]  5 C ohen A S.Paleolmi nology:The H istory and Evo lut ion of LakeSystem s.N ew Y ork:O xford U n iversity Press,2003.162~164
[29]  6 Sandgren P,Snowb all .IA pp lication of m ineral magnetic techn iquesto p aleo lmino logy.In:Last W M,Sm ol J P eds.Track ingE nvironm ental Change U sing Lak e Sed mi en ts(V o.l 2).D ordrech :tK luw er A cadem ic Pub lishers,2001.217~237
[30]  7 Thom pson R.Palaeolmi nology and p alaeom agn et ism.N ature,1973,242 :182~184
[31]  8 Thom pson R,Betterbee R W,O Su llivan P E e t al.M agn et icsuscep tibil ity of lak e sed mi en ts.L imnology and O cean og raphy,
[32]  19 75 ,20(5):687~698
[33]  9 O ld field F.M agnet ic m easurem en ts of recen t sed mi ents from B igM oose Lak e,A d irondack M oun tains,N Y.,U SA.Journal ofPa laeolimnology,1990,4:93~101
[34]  10 Peck J A,K ing J W,Colem an S M et al.A rock m agnetic recordfrom Lak e Baika,l S ib eria:E vidence for Late Q uaternary clmi atechange.Ea rth and P lanetary Sc ience L etters,1994,122(1~2):221~238
[35]  11 W illiam s T,Thouveny N,C reer K M et al.Palaeocl imat ics ign if ican ce of the 300k am ineralm agnetic record from th e sed mi en tsof Lac du Bou ch e,tFrance.Q ua terna ry S cience R eview s,1996,15:223~235
[36]  12 A llen J R M,Brandt U,Brau er A e t a l.R ap id environm entalchanges in sou thern Europe du ring th e last glacial period.N a tu re,
[37]  19 99 ,400:740~743
[38]  31 沈吉,王苏民,M atsum oto R等.内蒙古岱海古水温恢复及其古气候意义.中国科学(D辑),2001,31(12):1017~1023Shen J,i W ang Sum in,M atsum oto R et al.Q uan t itativereconstruct ion of the lake w ater paleotem peratu re of D aihai Lake,Inn erM ongolia,Ch ina and its s ign if ican ce in pa leoclmi ate.Sc iencein China(Series D),2002,45(9):792~800
[39]  32 J in X C.Lake in C h ina R esearch of Their Environm en .tBeijing:Ch ina O cean Press,1995.480~504
[40]  33 Tauxe L,L aB reque J L,D odson R et a .l(U)channels A newtechn ique for paleom agn et ic analys is of hyd rau lic p iston cores.EOS,
[41]  19 83 ,64(18):219
[42]  34 H a ilw ood E A.M agn etostratigraph ic resolu tion us ing th e 2G w holecorem agnetom ete:rA n expermi ental study,X?G en eral A ssem b lyof th e Eu ropean G eophys ical Society(A bstracts).Annua l ofG eophysica .l10,E dinbu rgh,1992.23
[43]  35 W eeks R J,L aj C,End ignoux L et a .lmI p rovem ents in long corem easurem en t techn iques:A pp lication in palaeom agnetism andpa laeoceanography.Geophy sical Journal Interna tional,1993,114:651~662
[44]  36 N agy E A,V alet J P.N ew advances for paleom agn et ic stud ies ofsed mi ent cores u sing U chann els.G eophysical Re sea rch L e tters,
[45]  19 93 ,20(8):671-674
[46]  37 T auxe L,W u G.N ormal ized rem an ence in sed mi ents of the w esternequatorial Pacif ic:R elative paleo inten sity of the geom agnetic field?Jou rnal of G eophysica l R esearch,1992,97(B8):12337~12350
[47]  38 Con stable C G,Parker R L.D econvo lut ion of long core paleom agnetic m easurem en ts:Sp lin e therapy for th e l inear prob lem.G eophysica l Journal In ternationa ,l1991,104:453~468
[48]  39 O da H,Shibuya H.D econvolut ion of long core paleom agnetic dataof O cean D rilling Program by A kaik e s Bayes ian In form ationC riterion m in im izat ion.Jou rnal of G eophysica l Research,1996,
[49]  10 1 :2815~2834
[50]  40 G uyodo Y J,Ch annell J M T,Thom as R G.D econvo lut ion ofU channel paleom agnetic data near geomagnetic reversals and shorteven ts.G eophysical R esearch L etters,2002,29(17):1845,do:i10 1029/2002G L014927
[51]  41 D earing J A,D ann R J L,H ay K e t al.Frequen cy depend entsu scept ib ility m easu rem ents of environm en tal materials.G eophysica lJou rnal In terna tional,1996,124:228~240

Full-Text

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133