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Fissure fills along faults: Variscan examples from Gower, South Wales

Published online by Cambridge University Press:  13 July 2009

V. WRIGHT ,
N. H. WOODCOCK  and
J. A. D. DICKSON
V. WRIGHT
Affiliation:
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK
N. H. WOODCOCK*
Affiliation:
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK
J. A. D. DICKSON
Affiliation:
Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK
*
*Author for correspondence: [email protected]
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Abstract

The extent to which persistent, rather than transient, fissures (wide planar voids) can exist along upper crustal faults is important in assessing fault permeability to mineral and hydrocarbon-bearing fluids. Variscan (late Carboniferous) faults cutting Dinantian (Lower Carboniferous) limestones on the Gower peninsula, South Wales, host clear evidence for fissures up to several metres wide. Evidence includes dendritic hematite growth and elongate calcite growth into open voids, spar ball and cockade breccia formation, laminated sediment infill and void-collapse breccias. Detailed mapping reveals cross-cutting geometries and brecciation of earlier fissure fills, showing that fissures were formed during, rather than after, active faulting. Fissures therefore probably formed by geometric mismatch between displaced fault walls, rather than by solution widening along inactive faults.

Keywords

fault brecciavoidveinCarboniferous
Type
Original Article
Information
Geological Magazine , Volume 146 , Issue 6 , November 2009 , pp. 890 - 902
Copyright
Copyright © Cambridge University Press 2009

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