The Anatomy of an Alkalic Porphyry Cu-Au System: Geology and Alteration at Northparkes Mines, NSW, Australia Adam Pacey1,2,*, Jamie J. Wilkinson2,1, Jeneta Owens3, Darren Priest3, David R. Cooke4,5 and Ian L. Millar6 1Department of Earth Science and Engineering, Imperial College London, South Kensington, London, SW7 2AZ, United Kingdom 2Department of Earth Sciences, Natural History Museum, Cromwell Road, London, SW7 5BD, United Kingdom 3NorthparKes Mines, PO Box 995, ParKes, New South Wales, 2870, Australia 4Centre for Ore Deposit and Earth Sciences (CODES), University of Tasmania, Hobart, Tasmania 7001, Australia 5Transforming the Mining Value Chain (TMVC), an Australia Research Council (ARC) Industrial Transformation Research Hub, University of Tasmania, Hobart, Tasmania 7001, Australia 6NERC Isotope Geosciences Laboratory, Keyworth, Nottingham, NG12 5GG, United Kingdom *Corresponding author:
[email protected] Keywords Northparkes, Macquarie Arc, porphyry deposit, propylitic alteration, potassic alteration, hydrothermal alteration, copper, gold Abstract The Late Ordovician-Early Silurian (~455-435 Ma) Northparkes system is a group of silica-saturated, alkalic porphyry deposits and prospects which developed within the Macquarie Island Arc. The system is host to a spectacular and diverse range of rocks and alteration-mineralization textures that facilitate a detailed understanding of its evolution, in particular into the nature and controls of porphyry-related propylitic alteration. The first intrusive phase at Northparkes is a pre- to early-mineralization pluton that underlies all the deposits and varies in composition from a biotite quartz monzonite (BQM) to alkali feldspar granite (AFG). Prior to total crystallization, this pluton was intruded by a more primitive quartz monzonite (QMZ) that marks the onset of a fertile fractionation series.