New Zealand Journal of Geology and Geophysics abstracts
Formation of authigenic Fe2+-bearing smectite-vermiculite during
terrestrial diagenesis, southern New Zealand
D. CRAW
D. W. SMITH
J. H. YOUNGSON
Geology Department
University of Otago
P.O. Box 56
Dunedin, New Zealand
Abstract Late Cretaceous to Quaternary terrestrial sediments
derived from fault scarps and actively growing folds in schist and greywacke
basement are locally preserved in Otago and South Canterbury, New Zealand.
Sediments are immature, sparsely carbonaceous, and generally poorly sorted and
have undergone little oxidation during rapid erosion and deposition cycles.
Mild oxidative alteration of sediment clasts in some horizons has resulted in
pseudomorphous replacement of detrital biotite and metamorphic chlorite in
greywacke clasts, and chlorite in schistose clasts, by a green, interlayered,
ferrous iron-bearing smectite-vermiculite mineral of variable composition.
Smectite-vermiculite compositions form a regular trend from low Si and Al, high
Fe and Mg to moderate Si and Al, to low Fe and Mg. The Fe
2+
smectite-vermiculite also occurs as pools in the matrix and small
veinlets, and as a cement intimately intergrown with fine-grained clastic
matrix. The smectite-vermiculite is a diagenetic product formed preferentially
in sedimentary horizons which are reduced and moderately acidic (pH 3.5-4.5),
neutral, or possibly alkaline.
There is a close association between the Fe2+ smectite-vermiculite
mineral and authigenic gold deposition; the smectite-vermiculite is
occasionally coated and impregnated with fine-grained (micrometre scale) gold.
Gold precipitation probably occurs by electroless deposition from groundwaters
that are undersaturated with respect to gold.
Keywords terrestrial sediments; authigenic
smectite-vermiculite; gold; Otago; Kyeburn Formation; Glentanner Formation;
Blue Spur Conglomerate; Maori Bottom Formation
New Zealand Journal of Geology and Geophysics, 1995, Vol. 38: 151-158
0028-8306/95/3802-0151 $2.50/0 (c) The Royal Society of New Zealand
1995
PDF file of entire paper: medium quality (2082K); (scanned from paper original: notes about this process)
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