Controls on the formation of a large Zn-Pb Irish-type deposit: evidence from the Navan halos

Abstract

IAEG Annual Conference 2017, Sligo, Ireland, 12-14 May 2017The mainly epigenetic Navan orebody is hosted by the Lower Carboniferous shallow water carbonate Pale Beds. Subordinate mineralization, hosted by submarine debris flows and the lowermost overlying basinal rocks, formed during seafloor exhalation and reaches ore grade in the Conglomerate Group Ore

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