
| DATE | Thursday, 26 June 2003 |
| MEETING TYPE | General Meeting |
| TIME | 6.15pm |
| VENUE | Fritz-Loewe Lecture Theatre, School of Earth Sciences, Melbourne University, cnr Swanston and Elgin Streets |
| PRELIMINARIES | Drinks and nibbles at 5.30 pm in the Tea Room, 4th Floor ($2 per person) |
| TITLE | The timing and origin of lead-zinc mineralisation in Ireland. |
| SPEAKER | Chris Reed of The University of Melbourne |
| ABSTRACT | The Lower Carboniferous
carbonate rocks of central and southern Ireland are host to a large number
of base-metal deposits. The sulphide mineralisation is concentrated on
the hanging walls of normal faults, at the base of the lowest non-argillaceous
carbonate (the Waulsortian Limestone). While much of the mineralisation
resembles Mississippi Valley-type mineralisation, many of the deposits
are classified as Irish-type deposits. This is a problematic classification
that requires an additional component of synsedimentary or near-surface
mineralisation. This talk evaluates the validity of the Irish-type model
by investigating the nature and timing of mineralisation at four localities
within the Irish ore-field. Significantly, there is no evidence to support
the near-surface component to the mineralisation and instead it is suggested
that the Irish mineralisation is entirely epigenetic. The thermal maturation
of the Irish ore-field and its implications for ore-stage temperatures
is also discussed. |