Cretaceous oblique extensional deformation and magma accumulation in the Fosdick Mountains migmatite-cored gneiss dome, West Antarctica

Tectonics

Volumn 29, Issue 4, 2010, Pages

  McFadden, R R ^a,b   Siddoway, C S ^c   Teyssier, C ^a   Fanning, C M ^d  

^a UNIVERSITY OF MINNESOTA   (United States)

^b SMITHSONIAN TROPICAL RESEARCH INSTITUTE   (Panama)

^c University of Colorado College of Nursing   (United States)

^d AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

GRANITE; LANDFORMS; LEAD; LEVEES; SHEAR DEFORMATION; SHELLFISH; SILICATE MINERALS; TOOLS; ZIRCON;

ANTARCTICA; CRYSTALLIZATION AGE; DETACHMENT FAULTING; DIATEXITE; EXTENSIONAL DEFORMATION; FOLIATION DEVELOPMENT; GNEISS DOME; HETEROGENEOUS DEFORMATION; LEUCOGRANITES; LEUCOSOMES; MELT FLOW; MID-CRETACEOUS; MIGMATITE; NEW ZEALAND; OBLIQUE EXTENSION; RIFT SYSTEMS; SCALE DOMAINS; SHEAR STRUCTURE; STRIKE-SLIP FAULT; STRUCTURAL RELATIONSHIP; TIME-SCALES; U-PB ZIRCON AGES;

DOMES;

CRETACEOUS; DEFORMATION; DETACHMENT FAULT; DIKE; DIORITE; DOME; EMPLACEMENT; EXHUMATION; EXTENSIONAL TECTONICS; GNEISS; GONDWANA; GRANITE; LITHOLOGY; MAGMA; MIGMATITE; STRIKE-SLIP FAULT;

ANTARCTICA; NEW ZEALAND; WEST ANTARCTICA;

EID: 77955549002     PISSN: 02787407     EISSN: None     Source Type: Journal    
DOI: 10.1029/2009TC002492     Document Type: Article

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