Monazite as an Exploration Tool for Iron Oxide-Copper-Gold Mineralisation in the Gawler Craton, South Australia

Minerals

June Hill¹  Adrienne Brotodewo²  Caroline Tiddy²  Diana Zivak²  David Giles²  Jim Hodgkison³  Mitchell Neumann³ 

[1] CSIRO Mineral Resources, ARRC, P.O. Box 1130, Bentley, WA 6102, Australia;Future Industries Institute, UniSA STEM, University of South Australia, Mawson Lakes, SA 5000, Australia;OZ Minerals Limited, P.O. Box 248, Adelaide Airport, Adelaide, SA 5950, Australia;

关键词: monazite;    exploration geochemistry;    IOCG;    Gawler Craton;   

DOI  :  10.3390/min11080809

来源: DOAJ

【 摘 要 】

The chemistry of hydrothermal monazite from the Carrapateena and Prominent Hill iron oxide-copper-gold (IOCG) deposits in the IOCG-rich Gawler Craton, South Australia, is used here to define geochemical criteria for IOCG exploration in the Gawler Craton as follows: Monazite associated with IOCG mineralisation: La + Ce > 63 wt% (where La > 22.5 wt% and Ce > 37 wt%), Y and/or Th < 1 wt% and Nd < 12.5 wt%; Intermediate composition monazite (between background and ore-related compositions): 45 wt% < La + Ce < 63 wt%, Y and/or Th < 1 wt%. Intermediate monazite compositions preserving Nd > 12.5 wt% are considered indicative of Carrapateena-style mineralisation; Background compositions: La + Ce < 45 wt% or Y or Th > 1 wt%. Mineralisation-related monazite compositions are recognised within monazite hosted within cover sequence materials that directly overly IOCG mineralisation at Carrapateena. Similar observations have been made at Prominent Hill. Recognition of these signatures within cover sequence materials demonstrates that the geochemical signatures can survive processes of weathering, erosion, transport and redeposition into younger cover sequence materials that overlie older, mineralised basement rocks. The monazite geochemical signatures therefore have the potential to be dispersed within the cover sequence, effectively increasing the geochemical footprint of mineralisation.

【 授权许可】

Unknown