Megasequence architecture of Taranaki, Wanganui, and King Country basins and Neogene progradation of two continental margin wedges across western New Zealand.

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Title

Megasequence architecture of Taranaki, Wanganui, and King Country basins and Neogene progradation of two continental margin wedges across western New Zealand.

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University of Waikato

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ResearchCommons@Waikato

Description

Taranaki, Wanganui and King Country basins (formerly North Wanganui Basin) have been regarded as discrete basins, but they contain a very similar Neogene sedimentary succession and much of their geological history is held in common. Analysis of the stratigraphic architecture of the fill of each basin reveals the occurrence of four 2nd order megasequences of tectonic origin. The oldest is the early-early Miocene (Otaian Stage) Mahoenui Group/megasequence, followed by the late-early Miocene (Al...

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Format

Research paper

Research format

Conference item

Date created

2002

URL

https://hdl.handle.net/10289/3619

Related subjects

Taranaki Basin / Wanganui Basin / King Country Basin / Taranki Fault / Matemateaonga Formation / Giant Foresets Formation / Mahoenui Group / Mokau Group

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This article has been published in Proceedings of New Zealand Petroleum Conference 2002, 24 – 27 February. © 2002 Kamp, P. J. J., Vonk, A. J., Bland, K. J., Griffin, A. G., Hayton, S., Hendy, A. J.W., ... Naish, T.

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