The Farsund intrusion (SW Norway): A marker of late-Sveconorwegian (Grenvillian) tectonism emplaced along a newly defined major shear zone

Journal of Structural Geology

Volumn 32, Issue 10, 2010, Pages 1500-1518

  Bolle, Olivier ^a,d   Diot, Hervé ^b   Liégeois, Jean Paul ^c   Vander Auwera, Jacqueline ^a  

^a UNIVERSITY OF LIÈGE   (Belgium)

^b UNIVERSITÉ DE LA ROCHELLE   (France)

^c ROYAL MUSEUM FOR CENTRAL AFRICA   (Belgium)

^d Research Associate from the FNRS   (Belgium)

Author keywords

Anisotropy of magnetic susceptibility; Charnockite; Granite emplacement; Gravity tectonism; Sveconorwegian orogen; Transtension

Indexed keywords

ANISOTROPY OF MAGNETIC SUSCEPTIBILITY; CHARNOCKITE; GRANITE EMPLACEMENT; GRAVITY TECTONISM; SVECONORWEGIAN OROGEN; TRANSTENSION;

GALLIUM; GRANITE; MAGNETIC ANISOTROPY; MAGNETIC SUSCEPTIBILITY; QUARTZ; TECTONICS;

STRUCTURAL GEOLOGY;

CONTINENTAL COLLISION; EMPLACEMENT; IGNEOUS INTRUSION; MAGMATISM; MAGNETIC ANISOTROPY; MAGNETIC SUSCEPTIBILITY; OROGENY; PETROFABRIC; PLUTON; SHEAR ZONE; STRUCTURAL CONTROL; SVECONORWEGIAN OROGENY; TECTONIC SETTING; TRANSTENSION;

NORWAY;

EID: 78649457377     PISSN: 01918141     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jsg.2010.04.003     Document Type: Article

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