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Origin of sulphur in metamorphosed stratabound mineralisation from the Argyll Group Dalradian of Scotland

Published online by Cambridge University Press:  03 November 2011

R. A. Scott ,
R. A. D. Pattrick  and
D. A. Polya
R. A. Scott
Affiliation:
R. A. Scott, Cambridge Arctic Shelf Programme, Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, U.K.
R. A. D. Pattrick
Affiliation:
R. A. D. Pattrick, Department of Geology, The University, Manchester M13 9PL, U.K.
D. A. Polya
Affiliation:
D. A. Polya, Department of Geology, The University, Manchester M13 9PL, U.K.
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Abstract

Sulphur isotopic data are presented for the four horizons of stratabound mineralisation in the Argyll Group Dalradian (Vendian) of the Central Highlands of Scotland. The styles of mineralisation reflect the stratigraphic and tectonic evolution of the Dalradian basin. The SEDEX-type Ba + (Zn + Pb) Loch Lyon Horizon has δ34S values for pyrite of +17% and for baryte of +27%. The baryte sulphur source was Dalradian sea-water although the values were modified by isotopic exchange with an H2S-rich metamorphic fluid derived from the surrounding graphitic schists. The sulphur source for sulphide in the horizon was probably the underlying strata; sulphide values were only slightly affected by metamorphism. Sulphides in the Pyrite Horizon are isotopically indistinguishable from those in the remainder of the volcanogenic Ben Lawers Schist Formation (0 ± 4%); these values suggest that, at least in the Tyndrum area, sulphides in the Pyrite Horizon are of igneous origin. VMS-type Cu + Zn + Pb mineralisation in the Ben Challum Quartzite Formation has a narrow range of values around + ll%. The likely source of this sulphide sulphur is reduced sea-water sulphate, the isotopic values remaining consistent owing to the buffering effect of anhydrite in the underlying calcium-rich rocks.

Keywords

Stratabound mineralisationmetamorphic re-equilibrationDalradiansulphur isotopes
Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 82 , Issue 2 , 1991 , pp. 91 - 98
Copyright
Copyright © Royal Society of Edinburgh 1991

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