收稿日期: 1998-07-20
修回日期: 1998-11-20
网络出版日期: 1999-04-01
RESEARCH PROGRESS IN REE TRACER FOR SEDIMENT SOURCE
Received date: 1998-07-20
Revised date: 1998-11-20
Online published: 1999-04-01
杨守业,李从先 . REE示踪沉积物物源研究进展[J]. 地球科学进展, 1999 , 14(2) : 164 -167 . DOI: 10.11867/j.issn.1001-8166.1999.02.0164
As an important tracer, REE is widely used to trace provenance of various sediments and sedimentary rocks. This paper firstly describes the characteristics of REE, then summarizes REE abundance and distribution patterns in seawater, freshwater , sedimentary rocks and sediments, and theirmain controlling factors. At lastthe application and problems of REE as a source rock tracer are also described in detail. Weathering of source rock can produce REE fractionation, especially during strong chemical weathering; Transport of particles and hydrodynamic sorting during formation of sediment also have potential influences on REE characters in sediment. REE abundance and patterns are different in different grain-sized sediments. It is generally regarded that clay has REE compositionmost close to source rock, whereas sandy sediment differentiates fromsource rock inREE composition, because detritusminerals can alsoobviously influence REE content and distribution patterns in sediment. REE normalizing and determining problems are discussed in the end of the paper.
Key words： REE; Provenance; Tracer; Sediment·
〔1〕Cullers R L, Barrett T, Carlson R,et al. REE and mineralogic changes in Holocene soil and stream sediment. Chem Geol,1987,63:275~297.
〔2〕Cullers R L , Basu A, Suttner L J. Geochemical signature of provenance in sand-size mineral in soil and stream near the tabacco root batholith, Montana, USA. Chem Geol, 1988,70:335~348.
〔3〕McLennan SM, Taylor S R. Sedimentary rocks and crustal evolution:tectonic setting and secular trands. The J Geol,1991,99:1~21.
〔4〕McLennan S M. Rare earth elements in sedimentary rocks:influence of provenance and sedimentary processes. In: Lipin B R , McKay G A,eds. Geochemistry and mineralogy of rare earth elements. Reviews in Mineralogy,1989,21:169~200.
〔5〕Taylor S R, McLennan SM. The continental crust:Its composition and evolution. Blackwell, 1985, 312.
〔6〕Girty GH.Provenance and depositional setting of Paleozoic chert andargillite,Sierra Nervada, California. JSedi Res, 1996, 66 (1):107~118.
〔7〕Grigsby J D. Detrital magnetite as a provenance indicator. J Sedi Petrol, 1990,60(6):940~951.
〔8〕Morton A C. Geochemical studies of detrital heavy minerals and their application to provenance research.In:Morton A C, eds. Development in sedimentary provenance studies,1991.31~45.
〔9〕Murray R W, Brink M R, Brumsack H J,et al. REE in Japen Sea sediments and diagenetic behavior of Ce/Ce*:Results from ODP Log 127. Geochim Cosmochim Acta, 1991,55:2 453~2 466.
〔10〕Murray R W. Chemical criteria to identify the depositional environment of chert: general principles and applications. Sedi Geol, 1994,90: 213~232.
〔11〕Byrne RH, KimK -H. Rare earth element scavening in seawater.Geochim Cosmochim.Acta, 1990,54:2 645~2 656.
〔12〕Lee J H, Byrne RH. Examination of comparative rare earth element complexation behavior using linear free-energy relationships. Geochim Cosmochim Acta, 1992,56:1 127~1 138.
〔13〕Lee J H, Byrne R H. Complexation of trivalent rare earth elements(Ce,Eu,Gd,Tb,Yb) by carbonate ions. Geochim Cosmochim Acta,1993, 57:295~302.
〔14〕Millero F J. Stability constants for the formation of rare earth inorganic complexes as a function of ionic strength. GeochimCosmochimActa, 1992,56:3 123~3 132.
〔15〕Cantrell KJ, Byrne RH. Rare earth element compexation by carbonate and oxalate ions. Geochim Cosmochim Acta, 1987, 51:597~605.
〔16〕Turner D R. The equilibrium speciation of dissolved components in freshwater and seawater at 25℃and 1 atm. GeochimCosmochimActa, 1981,45:855~881.
〔17〕Goldstein S J, Jacobsen S B. Rare earth elements in river waters.Earth and Planetary Science Letters, 1988,89:35~47.
〔18〕Sholkovitz E R, Jacobson S B. Ocean particle chemistry : the fractionation of REE between suspended particles and seawater. Geochim Cosmochim Acta, 1994,58:1 567~1 579.
〔19〕Piper D Z. Rare earth elements in the sedimentary cycle: a summary.Chem Geol, 1985,14:285~304.
〔20〕ElderfieldH, Upstill-Goddard R, Sholkovitz ER. The rare earth elements in rivers,estuaries and coastal seas and their significance to the composition of ocean waters. Geochim Cosmochim Acta, 1990,54:971~991.
〔21〕RollinsonHR. Using Geochemical Data. Lonman Scientific&Technical,1993.
〔22〕Gromet L P, Dymek R F, Haskin LA,et al. The“North American Shale Composite”: Its complilation, major and trace element characteristics. Geochim Cosmochim Acta, 1984,48:2 469~2 482.
〔23〕Haskin MA, HaskinLA. REE in European shales: Aredetermination. Science, 154, 507~509.
〔24〕Condie K C. Another look at REEs in shales. Geochim Cosmochim Acta, 1991,55:2 527~2 531.
〔25〕Sholkovitz E R. Rare earth elements in marine sediments and geochemical standards. Chemi Geol,1990,88:333~347.
〔26〕Sholkovitz ER. Rare earth elements in the sedimentsofthe North Atlantic Ocean,Amazon Delta, and East China Sea: Reinter-pretation of terrigenous input patterns to the oceans. Am J Sci, 1988,288:236~281.
〔27〕Nesbitt HS, Young G W. Petrogenesis of sediment in the absence of chemical weathering: effencts of abrasion and sorting on bulk composition and mineralogy. Sedimentology, 1996, 43:341~358.
〔28〕Nesbitt H W, MacRae N D, Kronberg B I. Amazon deep-sea fan muds: Light REE enriched products of extreme chemical weathering.Earth Planet Sci Lett, 1990, 100;118~123.
〔29〕Roaldest E. REE in Quaternary clays of the Numedal area,southern Norway. Lithos, 1973,6:349~372.
〔30〕杨忠芳,陈岳龙.陆源碎屑沉积作用对化学元素配分的制约.地质论评,1997,43(6):593~600.
〔31〕王中刚,于学元,赵振华,等.稀土元素地球化学.北京:科学出版社,1989.
〔32〕Suttner L J, Basu A. Climate and the origin of quartz arenite. J Sedi Petrol, 1981,51(4):1 235~1 246.
〔33〕Johnsson M J,Robert F S, Robert HM. First-cycle quartz arenite in the Orinoco River basin,Venezuela and Colombia. J Geol, 1988,96:263~277.
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