Superposed deformation in turbidites and syn-sedimentary slides of the tectonically active Miocene Waitemata Basin, northern New Zealand-Reference-Cited by-同舟云学术

Superposed deformation in turbidites and syn-sedimentary slides of the tectonically active Miocene Waitemata Basin, northern New Zealand

Published:2007-06 Issue:2 Volume:19 Page:199-216
ISSN:0950-091X
Container-title:Basin Research
language:en
Short-container-title:Basin Research

Author:

Spörli K. B.,Rowland J. V.

Publisher

Wiley

Subject

Geology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1365-2117.2007.00320.x/fullpdf

Reference74 articles.

1. H.B. Alldred (1980 ) Sedimentology and structure of the Waitemata Group, Wenderholm-Orewa section, North Auckland. Unpublished BSc Hons Thesis, University of Auckland, New Zealand. 66pp.

2. The Parnell Grit beds revisited: Are they all the products of sector collapse of western subaerial volcanoes of the Northland Volcanic Arc?

3. The Sedimentology Of The Waitemata Group In The Takapuna Section,Auckland

4. An Inter-Arc Flysch Basin in Northern New Zealand: Waitemata Group (Upper Oligocene to Lower Miocene)

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