New Zealand Journal of Geology and Geophysics abstracts
The elemental content of Niue Island soils as an indicator of their
origin
N. E.WHITEHEAD
Institute of Geological and Nuclear Sciences Ltd
P.O. Box 31 312
Lower Hutt, New Zealand
J. HUNT
D. LESLIE
P. RANKIN
Manaaki Whenua - Landcare Research
P.O. Box 31 902
Taita, Lower Hutt, New Zealand
Abstract The major and trace element contents of 241 Niue Island
lateritic soils were determined, mainly by X-ray fluorescence, to
deduce soil origins. The analyses showed very low SiO
2
content, and a high content of Mg, P, V, Cr, Sr, Y, Hg, and α-counts,
compared with other laterites worldwide. The distribution patterns are
consistent with derivation by weathering from calcite and dolomite
rather than from deposited volcanic ash. Weathering is a particularly
novel explanation for the origin of the relatively high content of P in
these soils. The soils contain a negative Ce anomaly, consistent with
an origin from seawater or coral, but not volcanic ash. If recent
results showing in situ formation of magnetite in soils are applicable,
the soil mineralogy is wholly consistent with an origin from
calcite/dolomite. An origin from calcite is also consistent with the
relative lack of volcanic ash on the seabed nearby, and very low
deposition of aeolian dust. The radioactivity content is consistent
neither with calcite/dolomite weathering, nor volcanic ash origin, but
may have originated, like a few of the stable elements, from rising
hydrothermal solutions.
Keywords Niue Island; weathering; cerium; phosphate;
chromium; yttrium; mercury; soils
Received 12 June 1991; published 25 June 1993
New Zealand Journal of Geology & Geophysics, 1991, Vol. 36:
243—255
0028Ð8306/06/3602—0243 ©The Royal Society of New Zealand 1991
PDF file of entire paper: medium quality
(1041K); (scanned from paper original: notes about this process).
Digitisation of this article from the printed journal was kindly
facilitated by the Geological Society of New Zealand
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