Logo image
Late Quaternary sea-level and tectonic changes in northeast Fiji
Journal article   Peer reviewed

Late Quaternary sea-level and tectonic changes in northeast Fiji

Patrick Nunn, C Ollier, G Hope, P Rodda, A Omura and W Richard Peltier
Marine Geology, Vol.187(3-4), pp.299-311
2002
url
https://doi.org/10.1016/S0025-3227(02)00296-7View
Published Version

Abstract

Pacific islands tectonics sea-level change Quaternary Holocene
The islands of northeast Fiji studied are all the emergent parts of the northern end of the Lau-Colville Ridge, a remnant island arc which has been rising for most of the Quaternary. Within the study area, investigations of coastal landforms (primarily emerged notches and shore platforms) and emerged coral reefs allow rates of tectonic movements to be calculated. The Vanuabalavu Island group is shown to have subsided during the late Quaternary while the area around is shown to have risen over the same time period. This disparity may be a result of tensional rifting associated with the continuing rotation of the Fiji Platform. © 2002 Elsevier Science B.V. All rights reserved.

Details

Metrics

InCites Highlights

These are selected metrics from InCites Benchmarking & Analytics tool, related to this output

Collaboration types
Domestic collaboration
International collaboration
Web Of Science research areas
Geosciences, Multidisciplinary
Oceanography

UN Sustainable Development Goals (SDGs)

This output has contributed to the advancement of the following goals:

#13 Climate Action

Source: InCites

Logo image