The geomorphology of the flanks of the Lord Howe Island volcano, Tasman Sea, Australia

Deep-Sea Research Part II: Topical Studies in Oceanography

Volumn 58, Issue 7-8, 2011, Pages 899-908

  Kennedy, D M ^a   Brooke, B P ^b   Woodroffe, C D ^c   Jones, B G ^c   Waikari, C ^d   Nichol, S ^b  

^a UNIVERSITY OF MELBOURNE   (Australia)

^b Marine and Coastal Environment Group   (Australia)

^c UNIVERSITY OF WOLLONGONG   (Australia)

^d VICTORIA UNIVERSITY OF WELLINGTON   (New Zealand)

Author keywords

High Island; Isotope; Lord Howe Rise; Slump; Tasman Sea; Volcano

Indexed keywords

AUSTRALIA; BACKSCATTER INTENSITY; CARBONATE SEDIMENTS; CONTINENTAL CRUSTS; GEOMORPHIC EVOLUTION; GLACIAL PERIOD; HIGH ISLAND; ISLAND VOLCANO; LATE TERTIARY; LORD HOWE RISE; MARINE EROSION; MARINE SEDIMENTS; MIOCENE; MULTI-BEAM; MULTIBEAM SONAR; OCEANIC CRUST; QUATERNARY SEDIMENTS; SEA FLOOR; SEDIMENT CORE; SLUMP; STABLE-ISOTOPE ANALYSIS; TASMAN SEA; TECTONIC STABILITY; VERTICAL STRESS; VOLCANIC EDIFICE;

ACOUSTIC ARRAYS; ANOXIC SEDIMENTS; BACKSCATTERING; BUILDINGS; EROSION; ISOTOPES; SEDIMENTOLOGY; SUBMARINE GEOLOGY; UNDERWATER ACOUSTICS;

VOLCANOES;

BATHYMETRY; CARBONATE; CONTINENTAL CRUST; DATA ACQUISITION; EROSION RATE; GEOMORPHOLOGICAL MAPPING; INSTABILITY; ISOTOPIC ANALYSIS; MARINE SEDIMENT; MIOCENE; MULTIBEAM SONAR; REEF FORMATION; SEAFLOOR; SLUMPING; STABILITY ANALYSIS; STABLE ISOTOPE; VOLCANIC ERUPTION; VOLCANISM; VOLCANOLOGY;

AUSTRALIA; LORD HOWE ISLAND; NEW SOUTH WALES; PACIFIC OCEAN; TASMAN SEA;

MOLLUSCA;

EID: 79952815969     PISSN: 09670645     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.dsr2.2010.10.046     Document Type: Article

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