Abstract
SUMMARY Existing maps of satellite (free-air) gravity and bathymetry, and the CRUST 2.0 global crustal structure model have been used to make new Bouguer gravity anomaly and crustal thickness maps of the SW Pacific region to analyse the region's crustal structure. The new maps clearly outline the limits of the rifted, largely submerged continent of Zealandia. The Bouguer gravity anomalies of ocean crust, large igneous provinces and backarc basins vary simply and predictably with age. The bathymetric Fiji Platform lies in a water depth of 19 km for the entire Fiji Platform, comparable to stretched and submerged parts of Zealandia. The question whether the continental crustal thickness of Fiji is due to its actually being a rifted part of Gondwana–Zealandia or due to enhanced Eocene–Pliocene magmatism remains open, but testable, with the latter more likely. Using the new accurate 3-D crustal thickness and published radiometric dating of lavas, we estimate that the magmatic portions of Southwest Pacific Cenozoic subduction-related arcs (three Kings, Tonga and Vanuatu) have grown at net volumes which vary from 263 to ∼1400 km3 km–1 with net addition rates of 17–31 km3 km–1 Ma–1.
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