Cenozoic reactivation of the great Glen Fault, Scotland: Additional evidence and possible causes

Journal of the Geological Society

Volumn 170, Issue 3, 2013, Pages 403-415

  Le Breton, E ^a,b   Cobbold, P R ^a   Zanella, A ^a  

^a UNIVERSITÉ DE RENNES 1   (France)

^b FREIE UNIVERSITÄT BERLIN   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

CALCITE VEINS; EARLY EOCENE; FAULT TREND; FRACTURE ZONE; LATE OLIGOCENE; MARINE STRATA; OVERPRESSURE; SEAFLOOR SPREADING;

SEDIMENTATION;

TECTONICS;

CALCITE; CALEDONIAN OROGENY; CENOZOIC; DISPLACEMENT; EXHUMATION; FRACTURE ZONE; GREAT GLEN FAULT; SEAFLOOR SPREADING; VEIN (GEOLOGY);

ATLANTIC OCEAN; GLEN MORE; HIGHLAND; MID-ATLANTIC RIDGE; MORAY FIRTH; SCOTLAND; UNITED KINGDOM;

EID: 84877587691     PISSN: 00167649     EISSN: None     Source Type: Journal    
DOI: 10.1144/jgs2012-067     Document Type: Article

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