Paleointensities on 8 ka obsidian from Mayor Island, New Zealand

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Title

Paleointensities on 8 ka obsidian from Mayor Island, New Zealand

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Directory of Open Access Journals

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Directory of Open Access Journals

Description

The 8 ka BP (6050 BCE) pantelleritic obsidian flow on Mayor Island, Bay of Plenty, New Zealand, has been investigated using 30 samples from two sites. Due to a very high paramagnetic/ferromagnetic ratio, it was not possible to determine the remanence carriers. This is despite the fact that the samples were studied intensively at low, room, and high temperatures. We infer that a stable remanence within the samples is carried by single- or close to single-domain particles. Experiments to determ...

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Format

Research paper

Date created

2011-11-01

Creator

A. Ferk / R. Leonhardt / K.-U. Hess / D. B. Dingwell

Contributing partner

Solid Earth

URL

http://www.solid-earth.net/2/259/2011/se-2-259-2011.pdf

Related subjects

Science / Geology / Stratigraphy / Petrology / Dynamic and structural geology

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