Quaternary volcanism on Manus and M'buke Islands.

A. L. Jaques

Research output: Chapter in Book/Report/Conference proceedingChapterpeer-review

4 Citations (Scopus)

Abstract

Quaternary basalt is widely distributed around a caldera that forms Southwest Bay in SW Manus Island. The basalts are of transitional to mildly alkaline composition, rich in TiO2, Zr, Nb, and light rare-earth elements, and resemble the incompatible-element-enriched tholeiites of oceanic islands such as Hawaii and Iceland. A change from island-arc (plate-boundary) igneous activity in the Tertiary to ocean-island-type (intraplate) volcanism in the Quaternary, reflects a striking change in tectonic setting thought to have resulted from left-lateral translation of Manus Island and New Ireland past New Britain. The Quaternary intraplate volcanism of Southwest Bay, M'Buke and Johnstone Islands, and the St Andrew Strait Islands may be controlled by a NW-trending fracture system, but alternatively may represent a 'hot spot' trace.-Author

Original languageEnglish
Title of host publicationCooke-Ravian Volume of Volcanological Papers, Geological Survey of Papua New Guinea Memoirs
Place of PublicationPort Moresby
PublisherGeological Survey of Papua New Guinea
Pages213-219
Number of pages7
Publication statusPublished - 1981
Externally publishedYes

Publication series

NameCooke-Ravian Volume of Volcanological Papers

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