Delayed Subsidence After Rifting and a Record of Breakup for Northwestern Zealandia

Author:

Boston Brian1ORCID,Nakamura Yasuyuki1,Gallais Flora1,Hackney Ron2ORCID,Fujie Gou1ORCID,Kodaira Shuichi1ORCID,Miura Seiichi1,Kaiho Yuka1,Saito Saneatsu3,Shiraishi Kazuya3ORCID,Yamada Yasuhiro3

Affiliation:

1. Research and Development Center for Earthquake and TsunamiJapan Agency for Marine‐Earth Science and Technology Yokohama Japan

2. Geoscience Australia Canberra ACT Australia

3. Research and Development Center for Ocean Drilling ScienceJapan Agency for Marine‐Earth Science and Technology Yokohama Japan

Funder

Japan Agency for Marine-Earth Science and Technology

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference77 articles.

1. Origin of the New Caledonian ophiolites based on a French–Australian Seismic Transect

2. Seismic stratigraphic record of transition from Mesozoic subduction to continental breakup in the Zealandia sector of eastern Gondwana

3. Stratigraphy of the southern Norfolk Ridge and the Reinga Basin: A record of initiation of Tonga–Kermadec–Northland subduction in the southwest Pacific

4. Global Bathymetry and Elevation Data at 30 Arc Seconds Resolution: SRTM30_PLUS

5. Bernardel G. Lafoy Y. Van De Beuque S. Missegue F. &Nercessian A.(1999).Preliminary results from AGSO law of the sea cruise 206: An Australian/French collaborative deep‐seismic marine survey in the Lord Howe Rise/New Caledonia region.Australian Geological Survey Organisation Record 1999(14).

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