1994
DOI: 10.1180/claymin.1994.029.2.12
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Palygorskite in the Regolith from the Mokau District, North Island, New Zealand

Abstract: A B S T R A C T: 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~ intervals to 700~ Palygorskite 'anhydride' formed at 400~ and sillimanite formed at 500~ The palygorskite is believed to have formed in joints in limestone of Upper Oligocene age (Dnntroonian) prior to uplift and subsequent weathering. It is highly crystalline, and appears not to have altered or weat… Show more

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Cited by 4 publications
(1 citation statement)
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“…However, records offibers 0.03 to OiIum (30 -100 nm) in diameter are fairly common (Serratosa 1979;Botha and Hughes 1992;Eee and Coban 1994;Kirkman and Wallace 1994;Gehring et aI. 1995;Singer et al 1995 Rossi and Cai'iaveras, (1999).…”
Section: Sepiolite and Palygorskitementioning
confidence: 99%
“…However, records offibers 0.03 to OiIum (30 -100 nm) in diameter are fairly common (Serratosa 1979;Botha and Hughes 1992;Eee and Coban 1994;Kirkman and Wallace 1994;Gehring et aI. 1995;Singer et al 1995 Rossi and Cai'iaveras, (1999).…”
Section: Sepiolite and Palygorskitementioning
confidence: 99%