沉积物物源分析研究进展Prospects of Sediment Provenance Analysis
徐亚军;杜远生;杨江海;
摘要(Abstract):
沉积物物源分析是盆地分析的重要内容,是再现沉积盆地演化、恢复古环境的重要依据。简要回顾了物源分析的发展史,重点介绍了重矿物、沉积物地球化学和同位素测年技术在物源分析中的应用和发展,指出了物源分析中尚需解决的地质问题。在强调多种方法综合使用的同时,也应考虑构造背景和化学风化作用。
关键词(KeyWords): 物源分析;沉积地球化学;沉积盆地分析
基金项目(Foundation): 国家自然科学基金项目(40672080)
作者(Author): 徐亚军;杜远生;杨江海;
Email:
DOI:
参考文献(References):
- [1]杜远生,颜佳新,韩欣.造山带沉积地质学研究的新进展[J].地质科技情报,1995,14(1):29-34.
- [2]Dickinson W R,Suczek C A.Plate tectonics and sandstonecompositions[J].Bull.Am.Ass.Petrol.Geol.,1979,63(2):2 164-2 182.
- [3]Dickinson W R,Valloni R.Plate settings and provenance ofsands in modern oceans[J].Geology,1980,8:82-86.
- [4]Dickinson W R.Provenance of North American Phanerozoicsandstones in relation to tectonic setting[J].Bull.Geol.Soc.Am.,1983,94:222-235.
- [5]Brijraj K D,Al-Mikhlafi AS,Kaur P.Geochemistry of Man-sar Lake sedi ments,Jammu,India:I mplicationfor source-areaweathering,provenance,and tectonic setting[J].Journal ofAsian Earth Sciences,2006,26:649-668.
- [6]She Zhenbing,Ma Changqian,Mason R,et al.Provenance ofthe Triassic Songpan-Ganzi flysch,West China[J].ChemicalGeology,2006,231:159-175.
- [7]Schwab F L.Evolution of the western continental margin,French-Italian Alps:Sandstone mineralogy as anindex of platetectonic setting[J].J.Geol.,1981,89(3):349-368.
- [8]Schwab F L.Sedi mentary signatures of foreland basin assem-blages:Real or counterfect?Foreland basin[J].Spec.Publ.Int.Ass.Sedi ment,1986,8:395-410.
- [9]Crook K A W.Lithogenesis and geotectonics:The significanceof composition in flysch arenites(gray wackes)[M]∥Dott RH,Shaver R H.Modern and ancient geosynclinal sedi menta-tion.Tulsa:SEPMSpec.Publ.,1974,19:304-310.
- [10]Maynard J B.Composition of modern deep-sea sands fromarc-related basins[M]∥Leggtt J K.Trench-forearc geology.Ox-ford:Blackwall Scientific Publication,1982:551-562.
- [11]Bhatia M R.Plate tectonics and geochemical composition ofsandstone[J].J.Geol.,1983,91(6):611-627.
- [12]Bhatia M R,Crook K A W.Trace element characteristics ofgyaywake and tectonic of sedi mentary basins[J].Cureau.Mineral.Petrol.,1986,92:181-193.
- [13]Roser B P,Korsch R J.Determination of tectonic setting ofsandstone mudstone suites using Si O2content and K2O/Na2Oratio[J].J.Geol.,1986,94(5):635-650.
- [14]和政军.砂岩碎屑组分与板块构造位置关系的研究现状[J].地质科技情报,1990,9(4):7-12.
- [15]方国庆.一个用于推断复理石形成时板块构造背景的判别图[J].西北地质科学,1993,14(1):121-125.
- [16]李曰俊,孙龙德,龚福华,等.藏北查桑上三叠统复理石沉积大地构造背景的初步探讨[J].岩石学报,2000,16(3):443-448.
- [17]李双应,李任伟,王道轩,等.大别山北缘凤凰台组砾石地球化学特征及源区构造环境[J].沉积学报,2005,23(3):380-388.
- [18]杨江海,杜远生,朱杰.甘肃省景泰正路下志留统复理石杂砂岩沉积地球化学特征[J].地质科技情报,2006,25(5):27-31.
- [19]Leterrier J,Maury R,Thonon P,et al.Clinopyroxene com-position as a method of identification of the magmatic affinitiesof paleo-volcanic series[J].Earth Planet.Sci.Lett.,1982,59:139-154.
- [20]Morton A C.A new approach to provenance studies-electronmicroprobe analysis of detrital garnets from Middle Jurassicsandstones of the northern North sea[J].Sedi mentology,1985,32:553-566.
- [21]李任伟,李忠,江茂生,等.合肥盆地碎屑石榴石组成及其对源区恢复和地层对比的意义[J].中国科学:D辑,2000,30(增刊);91-98.
- [22]Morton A C,Hurst A.Correlation of sandstones using heavyminerals:An example fromthe Statfjord Formation of the Sn-orre Field,northern North Sea[M]∥Dunay R E,Hail wood EA.Nonbio stratigraphical methods of dating and correla-tion.[S.l.]:Geological Society Special Publication,1995,89:3-22.
- [23]Morton A C,Whitham A G,Fanning C M.Provenance ofLate Cretaceous to Paleocene submarine fan sandstones in theNorwegian Sea:Integration of heavy mineral,mineral chemicaland zircon age data[J].Sedi mentary Geology,2005,182:3-28.
- [24]Renata C,Sulovsky P,Bruce A P.Major and trace elementsin pyrope al mandine garnets as sedi ment provenance indicatorsof the Lower Carboniferous Cul m sedi ments,Drahany Up-lands,Bohemian Massif[J].Lithos,2005,82:51-70.
- [25]Spiegel C,Wolfgang S,Wolfgang F,et al.Nd and Sr isotopicratios and trace element geochemistry of epidote from theSwiss Molasse Basin as provenanceindicators:I mplications forthe reconstruction of the exhumation history of the CentralAlps[J].Chemical Geology,2002,189:231-250.
- [26]Cardona J P M,Gutie'rrez Mas J M,Sa'nchez B A,et al.Sur-face textures of heavy-mineral grains:A new contribution toprovenance studies[J].Sedi mentary Geology,2005,174:223-235.
- [27]Roser B P,Korsch R J.Provenance signatures of sandstone-mudstone suits determined using discri minant function analysisof major-element data[J].Chemical Geology,1988,67:119-139.
- [28]Taylor S R,Mclennan S M.The continental crust:Its compo-sition andevolution[M].Oxford:Blackwell Scientific Publica-tion,1985.
- [29]Cullers R L,Graf J.Rare earth elements in igneous rocks ofthe continental crust:Intermediate and silicic rocks,ore petro-genes[M]∥Henderson P.Rare-earth geochemistry.Amster-dam:Elsevier,1983:275-312.
- [30]McLennan S M,Hemming S,McDanial D K,et al.Geochem-ical approaches to sedi mentation,provenance,and tectonics[J].Geological Society of American Special Paper,1993,284:21-40.
- [31]赵红格,刘池洋.物源分析方法与研究进展[J].沉积学报,2003,21(3):409-415.
- [32]Mark W H,Andrew C M.Evaluation of sedi ment provenanceusing magnetic mineral inclusions in clastic silicates:Compari-son with heavy mineral analysis[J].Sedi mentary Geology,2004,171:13-36.
- [33]D rra W,Floydb P A,Leveridge B E.U-Pb ages and geo-chemistry of granite pebbles fromthe Devonian Menaver con-glomerate,Lizard peninsula:Provenance of Rhenohercynianflysch of SW England[J].Sedi mentary Geology,1999,124:131-147.
- [34]Monika A K,Artur K,Mariusz P,et al.Provenance i mplica-tions of Th-U-Pb electron microprobe ages fromdetrital mona-zite in the Carboniferous Upper Silesia Coal Basin,Poland[J].Lithos,2006,88:56-71.
- [35]Li Renwei,Li Shuangying,Jin Fuquan,et al.Provenance ofCarboniferous sedi mentary rocksinthe northern margin of Da-bie Mountains,central China and the tectonic significance:Constraints from trace elements,mineral chemistry andSHRI MP dating of zircons[J].Sedi mentary Geology,2004,166:245-264.
- [36]李任伟,万渝生,陈振宇,等.根据碎屑锆石SHRI MP U-Pb测年恢复早侏罗世大别造山带源区特征[J].中国科学:D辑,2004,34(4):320-328.
- [37]Darby B J,George G.Detrital zircon reference for the NorthChina block[J].Journal of Asian Earth Sciences,2006,26:637-648.
- [38]李忠,李任伟,孙枢,等.大别地块北缘侏罗系花岗岩类砾岩的Rb-Sr年代学特征[J].科学通报,2001,46(7):582-585.
- [39]陈俊,王鹤年.地球化学[M].北京:科学出版社,2004:141-152.
- [40]Goldstein S L,Nions R K O,Hamillton PJ.ASm-Ndisotop-ic study of at mospheric dusts and particulates from major riversystem[J].Earth Planet.Sci.Lett.,1984,70:221-236.
- [41]McLennan S M,Taylor S R.Continental freeboard,sedi men-tation rates and growth of continental crust[J].Nature,1983,306:169-172.
- [42]陈江峰,周泰禧,邢凤鸣.皖南浅变质岩和沉积岩的钕同位素及沉积物物源区[J].科学通报,1989,34(20):1 572-1 574.
- [43]Harald G D.A review of heavy minerals in clastic sedi mentswith case studies fromthe alluvial-fan through the nearshore-marine environments[J].Earth-Science Reviews,1998,45:103-132.
- [44]王岳军,范蔚茗,林舸.盆地沉积物示踪源区山脉隆升剥露的几种办法[J].地质科技情报,1999,18(2):85-89.
- [45]Nesbitt H W,Young G M.Formation and diagenesis of weath-ering profiles[J].J.Geol.,1989,97(2):129-147.
- [46]汪正江,陈洪德,张锦泉.物源分析的研究与展望[J].沉积与特提斯地质,2000,20(4):104-110.
- [47]王国灿.沉积物源区剥露历史分析的一种新途径——碎屑锆石和磷灰石裂变径迹热年代学[J].地质科技情报,2002,21(4):35-40.
- [48]陈衍景,杨忠芳,赵太平.微量元素示踪物源区和地壳成分的方法和现状[J].地质地球化学,1996,15(3):7-11.