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Palygorskite in the Regolith from the Mokau District, North Island, New Zealand

Published online by Cambridge University Press:  09 July 2018

J. H. Kirkman  and
R. C. Wallace
J. H. Kirkman
Affiliation:
Department of Soil Science, Massey University, Palmerston North, New Zealand
R. C. Wallace
Affiliation:
Department of Soil Science, Massey University, Palmerston North, New Zealand
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Abstract

Corrugated mats of palygorskite occurring in regolith overlying a fissured limestone were examined by X-ray diffraction, infrared spectroscopy, and electron optical techniques after heating at 50°C intervals to 700°C. Palygorskite ‘anhydride’ formed at 400°C and sillimanite formed at 500°C. The palygorskite is believed to have formed in joints in limestone of Upper Oligocene age (Duntroonian) prior to uplift and subsequent weathering. It is highly crystalline, and appears not to have altered or weathered since precipitation.

Type
Research Article
Information
Clay Minerals , Volume 29 , Issue 2 , June 1994 , pp. 265 - 272
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1994

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