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Abstract

INTRODUCTION
The precious metal zone at Que River is an area in the northern parts of the eastern footwall containing
anomalously high amounts of gold and silver relative to
base metals when compared to the sulphide orebodies and the rest of the stringer system. The results of earlier
work on the precious metal zone may be found in
McGoldrick & Large (1987) and Jenkins (1988).

In this report, the results of fluid inclusion
thermometric measurements on the precious metal zone
and parts of PQ lens are presented, and further
conclusions are drawn regarding the origins of the
precious metal zone.

Item Type:	Report (Technical Report)
Authors/Creators:	Jenkins, GW
Publisher:	University of Tasmania
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