首页> 外文学位 >An integrated geochemical, petrologic, geochronological, and metallogenic study of the Powder Horn Intrusive Suite and the associated Lodestar Prospect: A magmatic-hydrothermal auriferous breccia zone that links epithermal and porphyry systems, Northern Burin Peninsula, Newfoundland.
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An integrated geochemical, petrologic, geochronological, and metallogenic study of the Powder Horn Intrusive Suite and the associated Lodestar Prospect: A magmatic-hydrothermal auriferous breccia zone that links epithermal and porphyry systems, Northern Burin Peninsula, Newfoundland.

机译:粉末角侵入套件及其相关Lodestar前景的综合地球化学,岩石学,地球年代学和成矿研究:岩浆热液角砾岩角砾岩带,连接超热和斑岩系统,纽芬兰北部。

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摘要

The Lodestar Prospect is associated with the Powder Horn Intrusive Suite and comprises auriferous sulphide-oxide mineralized polylithic breccias which have a magmatic-hydrothermal or phreatomagmatic origin. The best grades obtained by exploration companies from chip-channel sampling of the breccia were 4.98 g/t Au and 14.8 g/t Ag over 15.9 m, along with one area that returned an assay of approximately 2.0% Zn. Earlier assays derived values of 6.13 g/t Au over 4.7 m and 4.91 g/t Au over 3 m. More recent channel samples 5.6 g/t Au over 8.5 m including 12.6 g/t Au over 1m.;The Powder Horn Intrusive Suite is a multi-phase intrusive suite, with both pre- and post-brecciation (mineralization) phases. Pre-mineralization rocks consist of (1) the late Neoproterozoic Musgravetown Group sedimentary rocks, which are hornfelsed close to the intrusion, (2) medium grained gabbro/diorite, and (3) minor felsic material; the gabbro phase has been U-Pb zircon dated at 603+/− 2 Ma. Post-mineralization phases include (1) fine grained gabbro/diorite, (2) felsic phases, and (3) diabase dykes; a felsic dyke has been U-Pb zircon dated at 605+/− 5 Ma. (Abstract shortened by UMI.).
机译:Lodestar Prospect与Powder Horn Intrusive Suite相关联,并且包括源自岩浆热液或吞噬岩浆的氧化金硫化物矿化的多角砾岩。勘探公司从角砾岩的碎屑通道采样中获得的最佳品位是在15.9 m上的4.98 g / t Au和14.8 g / t Ag,以及一个返回约2.0%Zn含量的区域。较早的分析得出的值在4.7 m上为6.13 g / t Au,在3 m上为4.91 g / t Au。较新的通道样本在8.5 m上的5.6 g / t Au包括在1m上的12.6 g / t Au。粉角侵入体套件是一个多相侵入体套件,具有前,后矿化阶段(矿化)。矿化前的岩石由(1)新元古代晚期的Musgravetown Group沉积岩组成,它们靠近侵入岩呈角铁状;(2)中粒辉长岩/闪长岩;(3)次要的长英质物质;辉长岩相是U-Pb锆石,日期为603 +/- 2 Ma。矿化后阶段包括(1)细粒辉长岩/闪长岩,(2)纤长相,(3)辉绿岩堤;一项长生岩脉是U-Pb锆石,日期为605 +/- 5 Ma。 (摘要由UMI缩短。)。

著录项

  • 作者

    Hinchey, John Glenn.;

  • 作者单位

    Memorial University of Newfoundland (Canada).;

  • 授予单位 Memorial University of Newfoundland (Canada).;
  • 学科 Geology.;Geochemistry.
  • 学位 M.Sc.
  • 年度 2001
  • 页码 285 p.
  • 总页数 285
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 普通生物学;
  • 关键词

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