GEOCHEMISTRY AND RELATIONSHIPS TO MINERALIZATION OF SOME IGNEOUS ROCKS FROM THE HARLECH DOME, WALES.

P. M. Allen*, D. C. Cooper, R. Fuge, W. J. Rea

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

6 Citations (Scopus)

Abstract

Forty-nine samples of intrusions, cutting both the Upper Cambrian and the Ordovician, together with 11 samples of Ordovician volcanic rocks from the eastern side of the Harlech Dome, were studied petrographically and analysed for major and trace elements (Cu, Pb, Zn, As, Mo, Ba, Zr). The rocks were divided petrographically into five groups and verified by discriminant analysis of the chemical data. The results show a pre-Arenig episode of sub-alkaline intermediate and basic igneous intrusion, which has much in common with activity associated with porphyry copper mineralization in island arc environments. There is some evidence of a genetic association between the intermediate intrusions and the copper mineralization at Coed-y Brenin.

Original languageEnglish
Pages (from-to)b100-b108
JournalTransactions of the Institution of Mining and Metallurgy, Section B: Applied Earth Science
Volume85
Publication statusPublished - 1976

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