收稿日期: 1995-12-12
修回日期: 1996-03-04
网络出版日期: 1996-09-01
CARBON ISOTOPES IN MANTLE
Received date: 1995-12-12
Revised date: 1996-03-04
Online published: 1996-09-01
储雪蕾 . 地慢的碳同位素[J]. 地球科学进展, 1996 , 11(5) : 446 -452 . DOI: 10.11867/j.issn.1001-8166.1996.05.0446
Recently,many carbon isotopic investigations for the mantle samples,such as diamond,kimberlites,carbonatites,oceanic basalts and mantle xenoliths,have shown that a very concentrated distribution is around -5‰,and a relatively weak distribution is from about -15‰ to -25‰ in the mantle carbon isotopes.This type of carbon isotopic distributions is difficult to explain by the current hypotheses,such as phase transformation of carboniferous matters,subduction of sedimentary carbon or mantle degassing,and so it is possible that the primordial mantle is heterogeneous in carbon isotopes.
Key words: Mantle; Carbon isotopes; Heterogeneity
[l] Craig H. The geochemistry of the stable carbon isotopes. Geochim Cosmochim Acta,1953,3:53-92.
[2] Wickman F E. The cycle of carbon and the stable carbon isotopes. Geochim Cosmochim Acta, 1956,9:136-153.
[3]陈锦石,陈文正.碳同位素地质学概论.北京:地质出版社,1982:157.
[4] Kyser T K. Stable isotope variations in the mantle. Reviews in Mineralogy,1986,16:491-559.
[5] Defines P. Mantle carbon;concentration,mode of ovcurrence, and isotopic composition. In:Schidlowski M et al.(eds). Early organic evolution:implications for mineral and energy resources. Berlin:Springer-Verlag. 1992. 133-146.
[6] Pineau F, Methez E A. Carbon isotopes in xenoliths from the Hualalai volcano, Hawaii, and the generation of isotopic variability. Geochim Cosmochim Acta, 1990,54:2117-2127.
[7]Galimov E M. The relation between formation conditions and variations in isotope composition of diamonds. Geochem Intern ,198 5,22(1):118-142.
[8] Jaques A L, O'Neill H St C,Smith C B. Diamondiferous peridotite xenoliths from the Argyle (AK1) lamproite pipe,Western Australia. Contrib Mineral Petrol,1990, 104:255-276.
[9]Defines P, Harris J W,Gurney J J. Carbon isotopic composition, nitrogen content and inclusion composition of diamonds from the Roberts Victor kimberlite, South Africa; evidence for 13C depletion in the mantle. Geochim Cosmochim Acta,1987,51:1227-1243.
[10]Defines P, Harris J W,Robinson D N, et al. Carbon and oxygen isotope variations in diamond and graphite eclogites from Orapa,Botswana. Geochim Cosmochim Acta,1991,55:515-524.
[11][Roedder E. Liquid CO2 in olivine-bearing nodules and phenocrysts in basalts. Am Mineral, 1965,50: 1746-1786.
[12]Murck B W,Burruss R C, Hollister L S. Phase equilibris in fluid inclusions in ultramafic xenoliths. Am Mineral,1978,63:40-46.
[13]Bergman S C,Dubessy J. CO2-CO fluid inclusions in a composite peridotite xenolith:implications for upper mantle oxygen fugacity. Contrib Mineral Petrol,1984, 85:1-13.
[14]Nadeau S,Pineau F, Javoy M,et al. Carbon concentrations and isotopic ratios in fluid-inclusion-bearing upper-mantle xenoliths among the northwestern margin of North America. Chem Geol, 1990,81:271-297.
[15]Porcelli D R,O'Nions R K, Galer S J G, et al. Isotopic relationships of volatile and lithophile trace elements in contimental ultramafic xenoliths. Contrib Mineral Petrol,1992,110:528-538.
[16]储雪雷,樊棋诚,刘若新,等.中国东部新生代玄武岩中超镁铁质捕虏体的CO2包裹体的碳、氧同位素初步研究.科学通报,1995, 40(1): 62-64.
[17] Ohmoto H. Stable isotope geochemistry of ore deposits. Reviews in Mineralogy, 1986,16:431-559.
[18] Milledge H J, Mendelssofin M J, Seal M, et al. Carbon isotopic variation in spectral type 1(I diamonds. Nature, 1983,303:791一792.
[19] Kessen S E,Ringwood A E. Slab-mantle interactions, 2. the formation of diamonds. Chem Geol, 1989,78:97-118.
[20] Holland H D. The chemistry of the atmosphere and oceans. New York:J. Wiley and Sons, 1978. 351.
[21] Sobolev N V,Shatsky V S. Diamond inclusions in garnets from metamorphic rocks: a new environment for diamond formation. Nature,1990,343: 742-745.
[22] Javoy M,Pineau F, Iiyama I. Experimental determination of the isotopic fractionation between gaseous CO2 and carbon dissolved in tholeiitic magma. Contrib Mineral Petrol, 1978,67:35-39.
[23] Defines P. Regularities in the 13C and nitrogen content of the mantle revealed through studies of diamonds and the chemistry of their inclusions. In:Ext Abstr Worksh Diamonds, 28th Int Geol Congr, Washington D C. 1989. 18-20.
[24] Defines P. Stable isotope variations in carbonatites. In: Bell K (ed).Carbonatites-genesis and evolution. 1989. 301-359.
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