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Volumn 13, Issue 4, 2001, Pages 305-312

Magma homogenization during anatexis, ascent and/or emplacement? Constraints from the Variscan Weinsberg Granites

Author keywords

[No Author keywords available]

Indexed keywords

ANATEXIS; GRANITE; ISOTOPIC COMPOSITION; MAGMA;

EID: 0035655873     PISSN: 09544879     EISSN: None     Source Type: Journal    
DOI: 10.1046/j.1365-3121.2001.00365.x     Document Type: Article
Times cited : (36)

References (47)
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  • 8
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    • Isotopic disequilibrium during rapid crustal anatexis: Implications for petrogenetic studies of magmatic processes
    • (2000) Chem. Geol , vol.162 , pp. 169-191
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  • 17
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  • 21
    • 0342804520 scopus 로고    scopus 로고
    • Post-collisional granite generation and HT/LP metamorphism by radiogenic heating: The Variscan South Bohemian Batholith
    • London
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    • Gerdes, A.1    Wörner, G.2    Henk, A.3
  • 32
    • 0024483733 scopus 로고
    • The Moldanubian granitoid plutons of Austria: Chemical and isotopic studies bearing on their environmental setting
    • (1989) Chem. Geol , vol.76 , pp. 41-55
    • Liew, T.C.1    Finger, F.2    Hock, V.3
  • 36
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    • A model for monazite/melt equilibrium and applications to the generation of granitic magmas
    • (1993) Chem. Geol , vol.110 , pp. 127-146
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  • 46
    • 0030775451 scopus 로고    scopus 로고
    • Diapir-driven crustal convection: Decompression melting, renewal of the magma source and the origin of nested plutons
    • (1997) Tectonophysics , vol.271 , pp. 217-229
    • Weinberg, R.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.