“Straightening out” the Ohura Fault, North Wanganui Basin, New Zealand

P. J. Crosdale Geology Department, The University of Auckland, Private Bag 92 019, Auckland, New Zealand; Department of Earth Sciences, James Cook University, Townsville, Q, 4811, Australia

K. Regenauer Geology Department, The University of Auckland, Private Bag 92 019, Auckland, New Zealand; Graduiertenkolleg, Geomar, Kiel, 24148, Federal Republic of Germany

Abstract

The Ohura Fault, a major structural feature controlling the North Wanganui Basin, North Island, New Zealand, does not have the sinusoidal shape shown on 1:250 000 geological maps, but is a linear, NNE‐trending Y‐shear.

Keywords:

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Order Reprints Request Corporate Permissions

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

Request Academic Permissions

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.

“Straightening out” the Ohura Fault, North Wanganui Basin, New Zealand

Information for

Open access

Opportunities

Help and information

“Straightening out” the Ohura Fault, North Wanganui Basin, New Zealand

Abstract

Reprints and Corporate Permissions

Academic Permissions

Related research

To cite this article:

Download citation

Information for

Open access

Opportunities

Help and information

Keep up to date

Your download is now in progress and you may close this window

Login or register to access this feature