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Turbidites from the Clew Bay Complex, Ireland: provenance based on petrography, geochemistry and crustal residence values
Author(s) -
Harkin J.,
Williams D. M.,
Menuge J. F.,
Daly J. S.
Publication year - 1996
Publication title -
geological journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.721
H-Index - 54
eISSN - 1099-1034
pISSN - 0072-1050
DOI - 10.1002/(sici)1099-1034(199612)31:4<379::aid-gj719>3.0.co;2-x
Subject(s) - dalradian , provenance , geology , terrane , ordovician , detritus , petrography , geochemistry , foreland basin , ophiolite , accretionary wedge , laurentia , bay , basement , continental arc , passive margin , paleontology , metamorphic rock , volcanic rock , structural basin , oceanography , subduction , tectonics , archaeology , rift , history , volcano
The Clew Bay Complex in the Irish Caledonides represents a Caledonian element separating the Irish–Scottish Dalradian to the north from the South Mayo Ordovician arc basins to the south. The petrographic, geochemical and crustal residence characteristics of the Silurian sandstones within the complex are presented. Petrological analysis indicates that the sandstones were derived from a transitional continental provenance, possibly a passive continental margin or the cratonic flank of a foreland basin. Whole rock geochemistry confirms this provenance type and demonstrates the absence of any significant ophiolite detritus. Sm–Nd model ages indicate a possible derivation from Upper Dalradian or Torridonian rocks, although a mixed provenance may also be considered. These data indicate distinct differences between these turbidites and those of the nearby North Galway succession and suggest that the Clew Bay Complex could be regarded as a suspect terrane with respect to at least parts of the South Mayo arc zone. © 1996 John Wiley & Sons, Ltd.