An explanation for lycopod configuration, ‘Fossil Grove’ Victoria Park, Glasgow
- 1 May 1986
- journal article
- Published by Geological Society of London in Scottish Journal of Geology
- Vol. 22 (1), 77-83
- https://doi.org/10.1144/sjg22010077
Abstract
Molybdenite-bearing chlorite veins associated with siderite nodules have been discovered in Queyhouse talc quarry which is situated in the serpentinised basal part of the Shetland ophiolite on the island of Unst. The mineralization may be associated with acidic intrusive activity following the subduction and emplacement of the ophiolite complex.Keywords
This publication has 3 references indexed in Scilit:
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- XX. Note on the Nature of the Fossil Trees found at WhiteinchTransactions of the Geological Society of Glasgow, 1888
- On the Remains of a Fossil Forest in the Coal-measures at Wadsley, near SheffieldQuarterly Journal of the Geological Society, 1875