ADVANCES OF RESEARCH ON ENCLAVES IN INTERMEDIATE-ACIDIC MAGMATIC ROCKS
Received date: 1992-06-26
Revised date: 1992-10-19
Online published: 1993-07-01
徐夕生; 周新民; 王德滋 . 中酸性岩浆岩中岩石包体研究的新进展[J]. 地球科学进展, 1993 , 8(4) : 54 -58 . DOI: 10.11867/j.issn.1001-8166.1993.04.0054
Progresses of studies on enclaves within intermediate - acidic magmatic rocks of the resent decade, including the characteristics, model experiments of restite, quenched enclave and immiscible enclave, are reviewed comprehensively. The formation mechanisms and modele of the enclaves are also discussed in this paper.
Key words: enclaves; magmatic process; intermediate-acidic magmas
[1]Cocirta C et al.Ecemples de melange de magmas en contexte plutonique:les enclaves des tonalites-granodiorites du massitde Bono(Sardaigne Septentrionale).Can Jour Earth Sci,1989,26(6):1264-1281
[2] R.L.Rudnick ,何芝兰. 澳大利亚昆士兰的下地壳捕虏体:大陆玄武岩地壳深部同化作用和分离作用的证据[J]. 地质地球化学, 1987,(10) :14-27.
[3]徐夕生,周新民.花岗岩类中的岩石包体.南京大学学报〔地球科学版),1988,(1):234- 239
[4]Chappell B W,White A J R and Wyborn. The importance of residual source materoal(restite)in granite pertogenesis .Jour Petrol, 1987, (28) :1111-1138 .
[5]Wall V J et al. Medels for granitoid evolution and source composition .Jour Geol, 1987, 95 :731-749 .
[6]Chen Y D et al. Inclusions in three S--type granites from Southeastern Australia .Jour Petrol, 1989, 30(5) :1181-1218 .
[7]Chen Y D and Williams I S. Zircon inheritance in ma mafic inalusions from Bega batholith granites,Southeastern Australia:An ion microprobe study .Jour Geophy Res, 1990, 95(11) :17787-17796 .
[8]Domenick M A et al. Nd and Sr isotopic study of crustal and mantle inclusions from the Sierrs Nevada and implications for batholith petrogensia .Geological Society of America Bulletin, 1983, 94 :713-719 .
[9]White A J R and Chappell B W. Permigma and magma downunder .Geol Jour, 1990, 25(3-4) :221-225 .
[10]Venon R H.Restite,xenoliths and microgranitold enclaves in granites.Journal and Proceedings,Royal Society of New South Wales,1983,116:77-103
[11]Davidson J P et al. Small--scale disequilibrium in a magmatic inclusion and its more silicic host .Jour Geophy Res, 1990, 95(11) :17661-17675 .
[12]Campbell I H and Turner J S.The influence of viscosity of fountains in magma chambers.Jour Petrol,27:1130
[13]Frost T P and Mahood G A. Field,chemical and physical constraints on mafic-felsic magma interaction in the Lamark granodiorte,Sierra Nevada,California .Bull Geol Soc Am, 1987, 99 :272-291 .
[14]周新民,姚玉鹏,徐夕生. 浙东大衢山花岗岩中淬冷包体及其成因机制[J]. 岩石学报, 1992,3:234-241.
[15]Eichelberger J C. Vosiculation of mafic magma during replenishment of silica magma reservoirs .Nature, 1980, 288 :446-450 .
[16]Bender J F et al. The Cortlandt complex evidence for large--seale liquid immiscibility involving granodiorite and diorite magmas .Earth Planet Sci Lett, 1982, 58 :330-344 .
[17]Klaus Mezger,Rainer Altherr,Martin Okrusch,Friedhelm Henjes-Kunst,Hans Kreuzer. Genesis of acid/basic rock associations: a case study The Kallithea intrusive complex, Samos, Greece[J]. Contributions to Mineralogy and Petrology, 1985,90(4) .
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