上地幔物质组成的研究方法" /> 上地幔物质组成的研究方法" /> <span class="datatitle">上地幔物质组成的研究方法</span>
Please wait a minute...
img img
高级检索
地球科学进展  1993, Vol. 8 Issue (2): 53-58    DOI: 10.11867/j.issn.1001-8166.1993.02.0053
学术研究动态     
上地幔物质组成的研究方法
郑海飞1; 韩吟文2; 欧阳建平2
1.中国科学院地球化学研究所 贵阳 550002; 中国地质大学地球化学系 武汉 430074
 全文: PDF(1563 KB)  
摘要:

概述了目前地幔物质组成及其不均一性的地球化学研究方法和理论依据,其中包括:(1)互补法,(2)部分熔融模型反演法,(3)元素(或同位素)比值法,(4)元素丰度序列(模式)法。为了排除可能的干扰因素影响,本文还介绍了如何根据地球化学数据识别地壳物质的混染、岩浆或地幔混合及硫化物熔体分凝等作用的方法。

关键词: 地幔物质互补性部分熔融模型反演法元素比值法元素丰度序列法干扰因素识别    
收稿日期: 1992-04-30 出版日期: 1993-03-01
基金资助:

国家自然科学基金资助项目(4880150)

服务  
把本文推荐给朋友 上地幔物质组成的研究方法”的文章,特向您推荐。请打开下面的网址:http://www.adearth.ac.cn/CN/abstract/abstract3001.shtml" name="neirong"> 上地幔物质组成的研究方法">
加入引用管理器
E-mail Alert
RSS
作者相关文章  

引用本文:

郑海飞; 韩吟文; 欧阳建平. 上地幔物质组成的研究方法[J]. 地球科学进展, 1993, 8(2): 53-58.

链接本文:

http://www.adearth.ac.cn/CN/Y1993/V8/I2/53

[1]Ringwood.地幔的成分与岩石学,北京:地震出版社,1981,1-90
[2]路风香,邓晋福,鄂莫岚,辽宁宽甸黄椅山碱性玄武岩岩浆起源问题的讨论.地球科学,1981,(1),183-196
[3]邓晋福,路风香,鄂莫岚.汉诺坝玄武岩中超镁铁岩包体及其推导的上地幔性质.矿物学岩石学论丛,北京:地质出版社,1988,(4):18-30
[4]S S Sun. Chemical Composition and origin of the earth's primitive mantle. Geochim Cosmocim Acta.1982,46,1183-1188
[5]E Jagortz, H Palme,H H Baddenhausen,K Blum,M Cendales and M Dreibus. The abundance of major,minor and trace lelments in the earth's mantle as derived from primitive ultramafic nodules. Proc Lunar Sci Conf. 1979,10,2031-2050
[6]J E Minster and C J Alleger.Systenatic use of trace elements in igneous reocsses,part 3,inverse problem of batc melting in volcanic suites.1978,68:37-52
[7]H E Newsom,W M White,P K Jochum and A W Hofmann. Siderophile and Chalcophile element abundances in oceanic basalts,Pb isotope evolution and growth on the earth's core.Earth Planet Sci Lett,1988,(69):299-313
[8]W M White and J Patchett. Hf-Nd-Sr isotopes and incompatibale element abundances in island arcs:implications for magma origins and crust-mantle evolution. Earth Planet Sci Lett .1984,(67):167-185
[9]A W Hofmann and W M White. Ba and Cs in the earth'  s mantle. Z Naturforsch. 1983. 38a.  256-266
[10]K P Jochum, A W HoFmann, Ito E, H M Seufert and W M White. K, U and Th in mid-ocean ridge basalt glasses and heat production,K/U and K/Eb ratios in the mantla. Nature,  1984,(306):431-436
[11]S S Sun. Lead isotopic study of young volcanic rocks from mid-ocean ridgs, ocean islands and island arcs. Philos Trans R Soc London,1980,Ser. A297,409-445
[12]J A PeArce and J R Cann. Tectonic setting of basic volcanic rocks determined using trace element analyses,Earth Planet Soc Lett,1973,19:290-300
[13]M Wilsin And J P Davidson. The relative roles of crust and upper mantle in the generation of oceanic islan arc magmas.Phil Trans R Soc Lond,1984,A 310,664-669
[14]E M Piccrillo, L Civetta, R Petrini, A Longinelli, G Bellieni, Cormin-Chiaramonti P, Marpues L S and A J Melfi. Regional variations within the Parana flood basalts (Southern Brazil〕:Evidence for subcontinental mantle heterogeneity and crustal contami-nation. Chern Geol .1989,(75):103-122
[15]J B Marsh. Geochemica constraints on coupled assimilation and fractional crystallization involving upper crustal compositiorns and continental tholeiitic magma. Earth Planet Sci Lett.1989,(92):70-80
[16]W K Hart. Chemical and isotopic evidence for mixing between depleted and enriched mantle, northwestn USA.Geochim Cosmichim Acta.,  1985,(49):131-144
[17]P J McGoldrick, R R Keays and B B Scott. Thallium:a sensitive indicator of rock/seawater interaction and of sulfur saturation of silicate melt. Geochim Cosmochim Acat,1979,(43):1303-1311
[18] S J Barnes.The use of metal ratios in prospecting for platinum-group element deposits in mafic and ultramafic intrusions.Journal of Geochemical Exporation,1990,37(1):91-99
[19]张旗.如何正确使用玄武岩判别图.岩石学报,1990,(2):87-94

No related articles found!