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A vein occurrence of co-existing talc, saponite, and corrensite, Builth Wells, Wales

Published online by Cambridge University Press:  09 July 2018

L. A. J. Garvie  and
R. Metcalfe
L. A. J. Garvie
Affiliation:
Department of Physics and Astronomy, University of Glasgow, Glasgow, G12 8QQ, UK
R. Metcalfe
Affiliation:
Fluid Processes Group, British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK
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Abstract

Unique phyllosilicate assemblages occur in quartz-calcite veins cutting altered andesite at Builth Wells, UK. These veins show: (1) a central talc-dominated assemblage, grading into a saponite/corrensite/chlorite-dominated assemblage near their walls; (2) talc replacing calcite and quartz; and (3) closely associated blocky and fibrous saponite. Fibrous saponite occurs in narrow (<1 cm) fractures that extend for up to 1 m from major (⩽ 50 cm wide) talc-bearing veins. A thin halo (<5 mm) of wall-rock alteration, containing blocky saponite and minor corrensite, borders the fibrous saponite. These minerals may have originated when cooling, low-pH, quartz-saturated, Mg-rich fluid invaded pre-existing quartz/calcite veins. Quartz is replaced by talc where calcite dissolution caused the pH to increase. Wallrock alteration liberated Fe and Al to the fluid causing blocky saponite and corrensite to form. Fibrous saponite formed where lithostatic pressures were directed across hydraulic fractures.

Type
Research Article
Information
Clay Minerals , Volume 32 , Issue 2 , June 1997 , pp. 223 - 240
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1997

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