Relative elemental mobility during hydrothermal alteration of a basic sill, Isle of Skye, N.W. Scotland

作者: A. P. Dickin , N. W. Jones

DOI: 10.1007/BF01166609

关键词: Hydrothermal circulationIsotope analysisGeologyVein (geology)Mineral resource classificationSillCountry rockMetamorphismGeochemistry

摘要: In Sconser quarry, Isle of Skye, a thin Tertiary basic sill is cut by vertical veins which formed fluid conduits in major meteoric-hydrothermal system. order to study the relative mobility different elements during hydrothermal metamorphism, material adjacent large (6 mm wide) vein was into slices and subjected geochemical isotopic analysis.

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