The fast evolution of a crustal hot zone at the end of a transpressional regime: The Saint-Tropez peninsula granites and related dykes (Maures Massif, SE France)

Lithos

Volumn 162-163, Issue , 2013, Pages 195-220

  Duchesne, Jean Clair ^a   Liégeois, Jean Paul ^a,b   Bolle, Olivier ^a   Vander Auwera, Jacqueline ^a   Bruguier, Olivier ^c   Matukov, Dmitry I ^d   Sergeev, Sergey A ^d  

^a UNIVERSITY OF LIÈGE   (Belgium)

^b ROYAL MUSEUM FOR CENTRAL AFRICA   (Belgium)

^c UNIVERSITÉ MONTPELLIER 2   (France)

^d A P KARPINSKY RUSSIAN GEOLOGICAL RESEARCH INSTITUTE   (Russian Federation)

Author keywords

Geochemical modeling; Leucogranite; Mafic felsic magma interaction; Non CHARAC behavior; Shear zone plutonism; Variscan orogeny

Indexed keywords

ANDESITE; BASALT; CRUSTAL STRUCTURE; DEHYDRATION MELTING; DIABASE; DIKE; DIORITE; EMPLACEMENT; FELSIC ROCK; GEOCHRONOLOGY; GONDWANA; HERCYNIAN OROGENY; IGNEOUS GEOCHEMISTRY; LEUCOGRANITE; LITHOLOGY; MAFIC ROCK; MAGMA; MONAZITE; P-T CONDITIONS; PLUTON; PLUTONISM; SHEAR ZONE; TECTONICS; TRACE ELEMENT; TRANSPRESSION; ZIRCON;

FRANCE; MASSIF CENTRAL; MAURES MASSIF; PROVENCE-ALPES-COTE D'AZUR; TANNERON MASSIF; VAR;

EID: 84873977093     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2012.12.019     Document Type: Article

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