Fission-track ages of some tephras from cape kidnappers, hawke's bay, new zealand (note)

13Citations
Citations of this article
5Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

Four fission-track ages have been determined on glass shards from tephras of the Castlecliffian sequence at Cape Kidnappers. They are 0.85 ± 0.10 m.y. (the Kidnapper Tuff), 0.47 ± 0.09 m.y. (uppermost Mt Gordon Beds), 0.36 ± 0.08 m.y. (top of the Rabbit Gully Beds), and 0.32 ± 0.07 m.y. (base of the Trig. N Beds). © 1975 Taylor & Francis Group, LLC.

Cite

CITATION STYLE

APA

Seward, D. (1975). Fission-track ages of some tephras from cape kidnappers, hawke’s bay, new zealand (note). New Zealand Journal of Geology and Geophysics, 18(3), 507–510. https://doi.org/10.1080/00288306.1975.10421551

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free