Continental growth and recycling by accretion of deformed turbidite fans and remnant ocean basins: Examples from Neoproterozoic and Phanerozoic orogens

Memoir of the Geological Society of America

Volumn 200, Issue , 2007, Pages 63-92

  Gray, David R ^a   Foster, David A ^b   Maas, Roland ^a   Spaggiari, Catherine V ^c   Gregory, Robert T ^d   Goscombe, Ben ^e   Hoffmann, K H ^f  

^a UNIVERSITY OF MELBOURNE   (Australia)

^b UNIVERSITY OF FLORIDA   (United States)

^c GEOLOGICAL SURVEY OF WESTERN AUSTRALIA   (Australia)

^d SOUTHERN METHODIST UNIVERSITY   (United States)

^e UNIVERSITY OF ADELAIDE   (Australia)

^f GEOLOGICAL SURVEY OF NAMIBIA   (Namibia)

Author keywords

Continental growth; Convergent margins; Crustal recycling; Turbidites

Indexed keywords

BUILDINGS; DEFORMATION; SEA LEVEL; STRUCTURAL GEOLOGY; TECTONICS;

CONTINENTAL CRUSTS; CONVERGENT MARGIN; CRUSTAL RECYCLING; CRUSTAL THICKENINGS; MAGMATIC MATERIALS; SPATIAL AND TEMPORAL VARIATION; THINNED CONTINENTAL CRUST; TURBIDITES;

RECYCLING;

ACCRETION; CONTINENTAL CRUST; CONVERGENT MARGIN; CRUSTAL THICKENING; CRUSTAL THICKNESS; DEFORMATION; DETRITUS; LOWER CRUST; MAGMATISM; METAMORPHISM; OCEANIC CRUST; OROGENY; PALEOZOIC; PHANEROZOIC; RECYCLING; REGENERATION; SEA LEVEL; TURBIDITE;

AFRICA; DAMARA BELT; NAMIBIA; NEW ZEALAND; SOUTH ISLAND; TASMAN;

RAKAIA;

EID: 77949856371     PISSN: 00721069     EISSN: None     Source Type: Book Series    
DOI: 10.1130/2007.1200(05)     Document Type: Conference Paper

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