A unified model for gold mineralisation in accretionary orogens and implications for regional-scale exploration targeting methods |
| |
Authors: | Email author" target="_blank">Jon?M?A?HronskyEmail author David?I?Groves Robert?R?Loucks Graham?C?Begg |
| |
Institution: | (1) Western Mining Services, Suite 26, 17 Prowse St, West Perth, WA, 6005, Australia;(2) Centre for Exploration Targeting, University of Western Australia and Curtin University, 35 Stirling Highway, Crawley, WA, 6009, Australia;(3) Orebusters Pty. Ltd, 4 Handley Close, Leeming, WA, 6149, Australia;(4) Minerals Targeting International, Suite 26, 17 Prowse St, West Perth, WA, 6005, Australia;(5) GEMOC/CCFS, Department of Earth and Planetary Sciences, Macquarie University, Sydney, NSW, 2109, Australia |
| |
Abstract: | Accretionary orogens are the sites of long-lived convergent margin tectonics, both compressional and extensional. They are
also the hosts to the majority of the world’s important gold deposits. A very diverse range of deposit types occurs within
accretionary orogens, commonly in close proximity in space and time to each other. These include porphyry and associated high-sulphidation
Au–Cu–Ag deposits, classic low-sulphidation Au–Ag deposits, low-sulphidation Au deposits centred on alkalic intrusive complexes,
Carlin-type Au deposits, Au-rich volcanic-hosted massive sulphide deposits, orogenic Au deposits, intrusion-related Au deposits
and iron oxide Cu–Au deposits. Empirical patterns of spatial distribution of these deposits suggest there must be fundamental
generic controls on gold metallogeny. Various lines of evidence lead to the proposal that the underlying key generic factor
controlling accretionary orogen gold metallogeny is regional-scale, long-term, pre- and syn-subduction heterogeneous fertilisation
of the lithospheric mantle that becomes a source of mineralisation-associated arc magma or hydrothermal fluid components.
This process provides a gold-enriched reservoir that can be accessed later in a diverse range of tectonomagmatic settings.
Based on this concept, a unified model is proposed in which the formation of a major gold deposit of any type requires the
conjunction in time and space of three essential factors: a fertile upper-mantle source region, a favourable transient remobilisation
event, and favourable lithospheric-scale plumbing structure. This framework provides the basis for a practical regional-scale
targeting methodology that is applicable to data-poor regions. |
| |
Keywords: | |
本文献已被 SpringerLink 等数据库收录! |
|