Hikurangi Plateau: Crustal structure, rifted formation, and Gondwana subduction history-Reference-Cited by-同舟云学术

Hikurangi Plateau: Crustal structure, rifted formation, and Gondwana subduction history

Published:2008-07 Issue:7 Volume:9 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Davy Bryan¹,Hoernle Kaj²,Werner Reinhard³

Affiliation:

1. Institute of Geological and Nuclear Sciences; P.O. Box 30368,; Lower Hutt; New Zealand

2. IFM-GEOMAR; Wischhofstraße 1-3,; D-24148; Kiel; Germany

3. Tethys Geoconsulting GmbH; Wischhofstraße 1-3,; D-24148; Kiel; Germany

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference75 articles.

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2. Modelled palaeolatitudes for the Louisville hot spot and the Ontong Java Plateau;Antretter;Geol. Soc. Spec. Publ.,2004

3. Morphology and origin of the Osbourn Trough;Billen;J. Geophys. Res.,2000

4. Sound velocity-density parameters of sediment and rock from DSDP drill sites 315-318 on the Line Islands Chain, Manihiki Plateau, and Tuamotu Ridge in the Pacific Ocean;Boyce;Initial Rep. Deep Sea Drill. Proj.,1976

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