The generation of voluminous S-type granites in the Moldanubian unit, Bohemian Massif, by rapid isothermal exhumation of the metapelitic middle crust

Lithos

Volumn 121, Issue 1-4, 2011, Pages 25-40

  Žák, Jiií ^a,b   Verner, Kryštof ^a,b   Finger, Fritz ^c   Faryad, Shah Wali ^a   Chlupácová, Marta ^d   Veselovskỳ, František ^b  

^a CHARLES UNIVERSITY   (Czech Republic)

^b CZECH GEOLOGICAL SURVEY   (Czech Republic)

^c UNIVERSITY OF SALZBURG   (Austria)

^d NONE   (Czech Republic)

Author keywords

Anisotropy of magnetic susceptibility (AMS); Bohemian Massif; LP HT metamorphism; Moldanubian unit; Monazite geochronology; S type granite

Indexed keywords

CRUSTAL STRUCTURE; EXHUMATION; GEOCHRONOLOGY; MAGMA; MAGNETIC ANISOTROPY; MAGNETIC FABRIC; MIGMATITE; MIGMATIZATION; MONAZITE; MYLONITE; P-T CONDITIONS; S-TYPE ROCK; URANIUM-LEAD DATING;

BOHEMIAN MASSIF;

BRUNIA;

EID: 78650254737     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2010.10.002     Document Type: Article

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