Submarine paleoseismology of the northern Hikurangi subduction margin of New Zealand as deduced from Turbidite record since 16ka

Quaternary Science Reviews

Volumn 84, Issue , 2014, Pages 116-131

  Pouderoux, Hugo ^a,b   Proust, Jean Noël ^a   Lamarche, Geoffroy ^b  

^a UNIVERSITÉ DE RENNES 1   (France)

^b NATIONAL INSTITUTE OF WATER AND ATMOSPHERIC RESEARCH   (New Zealand)

Author keywords

Active margin; Earthquake hazard assessment; Paleoearthquake; Peak ground acceleration; Poverty Bay; Synchronous slope failures; Turbidite paleoseismology

Indexed keywords

ACTIVE MARGINS; EARTHQUAKE HAZARD; PALEOEARTHQUAKE; PALEOSEISMOLOGY; PEAK GROUND ACCELERATION; POVERTY BAYS; SLOPE FAILURE;

FAULTING; SLOPE STABILITY; STRUCTURAL ANALYSIS;

EARTHQUAKES;

ACCELERATION; CONTINENTAL SLOPE; EARTHQUAKE EPICENTER; EARTHQUAKE MAGNITUDE; EARTHQUAKE TRIGGER; HAZARD ASSESSMENT; PALEOSEISMICITY; RADIOCARBON DATING; SEDIMENTATION; SUBMARINE; TURBIDITY;

GISBORNE; HIKURANGI; NEW ZEALAND; NORTH ISLAND; NORTHLAND; POVERTY BAY;

EID: 84890290215     PISSN: 02773791     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.quascirev.2013.11.015     Document Type: Article

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