Extensional and magmatic nature of the Campbell Plateau and Great South Basin from deep crustal studies

Tectonophysics

Volumn 472, Issue 1-4, 2009, Pages 213-225

  Grobys, J W G ^a   Gohl, K ^a   Uenzelmann Neben, G ^a   Davy, B ^b   Barker, D ^b  

^a ALFRED WEGENER INSTITUTE FOR POLAR AND MARINE RESEARCH   (Germany)

^b GNS SCIENCE   (New Zealand)

Author keywords

Campbell Plateau; Crustal thinning; Great South Basin; Ocean bottom seismographs; Refraction methods; Rift zones

Indexed keywords

CAMPBELL PLATEAU; CRUSTAL THINNING; GREAT SOUTH BASIN; OCEAN-BOTTOM SEISMOGRAPHS; RIFT ZONES;

OCEAN ENGINEERING; OCEANOGRAPHY; REFRACTION; SEISMOLOGY; TECTONICS;

SEISMOGRAPHS;

CRUSTAL THICKNESS; CRUSTAL THINNING; EXTENSIONAL TECTONICS; LOWER CRUST; MAGMATISM; OCEAN BOTTOM SEISMOMETER; P-WAVE; RIFT ZONE; SEISMIC REFLECTION; SEISMIC REFRACTION; SEISMIC VELOCITY; SEISMOTECTONICS; VELOCITY STRUCTURE; WAVE VELOCITY;

AUSTRALASIA; CAMPBELL PLATEAU; CHALLENGER PLATEAU; GREAT SOUTH BASIN; LORD HOWE RISE; NEW ZEALAND; PACIFIC OCEAN; TASMAN SEA;

EID: 67349196736     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.tecto.2008.05.003     Document Type: Article

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