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Introduction to the Special Issue Devoted to Alkalic Porphyry Cu-Au and Epithermal Au Deposits

机译:碱性斑岩铜金和超热金矿床专刊简介

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This special issue is devoted to alkalic porphyry Cu-Au and epithermal Au deposits and focuses on two regions: British Columbia, Canada (Fig. 1), and the Southwest Pacific region (Australia and Papua New Guinea: Fig. 2). The special issue commences with a review of Triassic to Jurassic metallogeny of British Columbia (Logan and Mihalynuk, 2014), then documents ore zones from several alkalic deposits (Central zone, Galore Creek-Micko et al., 2014; Southwest zone, Galore Creek-Byrne and Tosdal, 2014; Northeast zone, Mt. Pol-ley-Pass et al., 2014; Lower Main zone, Lorraine-Bath et al., 2014; Mt. Milligan-Jago et al., 2014) and provides a comprehensive overview of mineralization in the Lorraine district (Devine et al., 2014). Four contributions document alkalic porphyry and epithermal deposits in New South Wales (Northparkes-Harris and Holcombe, 2014; Endeavour 41- Zukowski et al., 2014; Endeavour 42-Henry et al., 2014; Cadia-Harris et al., 2014). The final contribution uses the results of mapping and core logging in order to resolve the physical volcanology and hydrothermal evolution of the giant Ladolam alkalic epithermal gold deposit, Papua New Guinea (Blackwell et al., 2014). Eight of these papers are the outcome of a collaborative project between the Mineral Deposit Research Unit (MDRU) at the University of British Columbia, the Australian Research Councils Centre for Excellence in Ore Deposits (CODES) at the University of Tasmania, and industry partners. The remaining are based on work by the British Columbia Geological Survey (Logan and Mihalynuk, 2014), Teck Resources Ltd. (Devine et al., 2014), a research collaboration between CODES and Newcrest Mining Ltd. (Harris et al., 2014), and the University of Queensland (Harris and Holcombe, 2014).
机译:本期专刊是针对碱性斑岩性铜金和超热金矿床的,主要集中在两个地区:加拿大不列颠哥伦比亚省(图1)和西南太平洋地区(澳大利亚和巴布亚新几内亚:图2)。特刊开始于不列颠哥伦比亚省的三叠纪至侏罗纪成矿研究(Logan和Mihalynuk,2014年),然后记录了几种碱性矿床的矿区(中部地区,Galore Creek-Micko等人,2014年;西南地区,Galore Creek) -Byrne和Tosdal,2014;东北地区,Pol-ley-Pass山等人,2014; Lower Main地区,Lorraine-Bath等人,2014; Milligan-Jago等人,2014),并提供了洛林地区成矿的综合概述(Devine等,2014)。有四篇文献记录了新南威尔士州的碱性斑岩和超热沉积物(Northparkes-Harris和Holcombe,2014; Endeavor 41-Zukowski等,2014; Endeavor 42-Henry等,2014; Cadia-Harris等,2014) 。最后的贡献是利用测绘和岩心测井的结果来解决巴布亚新几内亚巨型Ladolam碱性超热金矿床的物理火山学和热液演化(Blackwell等人,2014)。其中八篇论文是不列颠哥伦比亚大学矿床研究部(MDRU),塔斯马尼亚大学澳大利亚研究委员会卓越矿床研究中心(CODES)与行业合作伙伴之间合作项目的成果。其余部分基于不列颠哥伦比亚省地质调查局(Logan和Mihalynuk,2014年),Teck资源有限公司(Devine等人,2014年)的工作,这是CODES与Newcrest Mining Ltd.(Harris等人,2014年)之间的研究合作。 )和昆士兰大学(Harris和Holcombe,2014年)。

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