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Clay- and zeolite-bearing Triassic sediments at Kaka Point, New Zealand; evidence of microbially influenced mineral formation from earliest diagenesis into the lowest grade of metamorphism

Jeans, C.V., Fallick, A.E., Fisher, M.J., Merriman, R.J., Corfield, R.M., and Manighetti, B. (1997) Clay- and zeolite-bearing Triassic sediments at Kaka Point, New Zealand; evidence of microbially influenced mineral formation from earliest diagenesis into the lowest grade of metamorphism. Clay Minerals, 32 (3). pp. 373-423. ISSN 0009-8558

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Publisher's URL: http://claymin.geoscienceworld.org/cgi/content/abstract/32/3/373

Abstract

The distribution, mineralogy, petrology and bulk and stable isotope chemistry of altered volcanic ash beds in the marine sediments of Mid-Triassic age (Etalian) at Kaka Point, New Zealand, are described and related to lithofacies and the geological processes controlling their development. Three varieties of altered ash occur in the Kaka Point sediments--porcellanite, claystone (bentonite) and albite-rich. Porcellanites are quartz-rich and may contain analcime and heulandite: they are restricted mainly to the on-shore facies. Claystones are rich in smectitic clay minerals and occur in both the on-shore and off-shore facies. They often contain diagenetic nodules of analcime, quartz, apatite and carbonates. The authigenic carbonates of the on-shore facies are variable in composition (sideritic, rhodochrositic, calcitic), whereas in the off-shore facies they consist only of calcite. The albite-rich lithology is very rare and is known only from the off-shore facies. The development of the porcellanite and albite-rich lithologies was restricted to slowly deposited, relatively coarse-grained ash sediments in which extensive interchange took place between the sediment's pore-waters and ambient seawater, resulting in enhanced microbial activity and high pH throughout the pore-waters of the suboxic zone beneath the water-sediment interface. The high pH increased the rate of volcanic ash hydrolysis and provided the conditions necessary for the precipitation of zeolite, feldspar and quartz. The development of smectitic claystones was associated with more rapid deposition and limited interchange between the pore-waters of the parent ash and ambient seawater. The pore-water alkalinity was generally lower and enhanced microbial activity and high pHs were restricted to patches of sediment at which quartz, analcime, apatite and carbonates formed diagenetic nodules. Modelling of the stable isotopes of the smectitic clays (delta 18 O, delta D) and diagenetic carbonates (delta 18 O, delta 13 C) suggest that: (1) ash argillization in the on-shore facies took place in brackish water ( approximately 25% meteoric water) at an average temperature of approximately 50 degrees C and in the off-shore facies in marine pore-waters ( approximately 1O% meteoric water) at approximately 40 degrees C: and (2) diagenetic carbonate precipitation in the near-shore facies took place at approximately 30 degrees C and in the off-shore facies at 60-80 degrees C. The pattern of ash alteration in the marine Triassic sediments at Kaka Point is considered to represent an early stage in the development of the zeolite pattern associated with the classic area of zeolite facies metamorphism in the Taringatura and Hokonui Hills.

Item Type:Article
Status:Published
Refereed:Yes
Glasgow Author(s):Fallick, Prof Anthony
Authors: Jeans, C.V., Fallick, A.E., Fisher, M.J., Merriman, R.J., Corfield, R.M., and Manighetti, B.
Subjects:Q Science > QE Geology
College/School:College of Science and Engineering > Scottish Universities Environmental Research Centre
Journal Name:Clay Minerals
Publisher:Mineralogical Society
ISSN:0009-8558
ISSN (Online):1471-8030

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