Granitoid gneisses with relict orbicular metagranitoids from the Varied Group of the southern Bohemian Massif Moldanubicum: Protolith derived from melting of Archaean crust?

Journal of the Czech Geological Society

Volumn 48, Issue 1-2, 2003, Pages 100-101

  Patocka F ^a   Kachlik V ^b   Dostal, J ^c   Frana J ^d  

^a INSTITUTE OF GEOLOGY   (Czech Republic)

^b CHARLES UNIVERSITY   (Czech Republic)

^c SAINT MARY S UNIVERSITY   (Canada)

^d NUCLEAR PHYSICS INSTITUTE   (Czech Republic)

Author keywords

[No Author keywords available]

Indexed keywords

AMPHIBOLITE FACIES; ARCHEAN; CRUST; GNEISS; GRANITOID; MELTING;

CZECHOSLOVAKIA;

EID: 0041381276     PISSN: 12108197     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (12)

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2. Fiala, J. - Fuchs, G. - Wendt, J. I. (1995): Moldanubian zone: stratigraphy. - In: Dallmeyer, R. D. - Franke, W. - Weber, K. (eds): Pre-Permian Geology of Central and Eastern Europe, 417-428, Springer Verlag. Berlin.
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8. nd ed.). - J. Wiley and Sons, London.
9. Candie, K. C. (1997): Plate tectonics and crustal evolution. - Elsevier, Amsterdam.
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