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Magmatic Platinum Group Element Environments in Canada: Present and Future Exploration Target Areas.


Magmatic Platinum Group Element Environments in Canada: Present and Future Exploration Target Areas by Larry Hulbert Geological Association of Canada The Geological Association of Canada promotes and develops the geological sciences in Canada. The organization holds conferences, meetings and exhibitions for the discussion of geological problems and the exchange of views in matters related to geology.  c/o Department of Earth Sciences Memorial University of Newfoundland Memorial University of Newfoundland, at St. John's, N.L., Canada; provincially supported; coeducational; founded 1925 as Memorial Univ. College. It achieved university status in 1949.  St. John's, Newfoundland A1B 3X5 www.gac.ca Special Publication, CD-format, $25.00

A few years ago I had the opportunity to attend an oral version of this presentation. I remember an inspiring talk, full of relevant facts and data, delivered with inspiration and enthusiasm by a dedicated professional who was presenting a significant part of his life's work. Included in this CD is a vastly expanded version of the original lecture, including 202 images (slides) many of these with attached, helpful and informative speakers notes, an extended abstract and a list of references. The author promises that the user of this CD will not only become knowledgeable about Platinum Group Elements (PGE PGE Pacific Gas and Electric Company
PGE Portland General Electric
PGE Prostaglandin E
PGE Platinum Group Elements
PGE Pacific Great Eastern (Railroad)
PGE Phenyl Glycidyl Ether
PGE Perfect Girl Evolution
) and their significance to our civilization and way of life, but also become convinced that Canada is endowed with the geology that will make it "the world's next major source of PGE". A tall order, one may think, bearing in mind that Canada currently produces <10% of the world's PGEs. However, this is exactly the impression one is left with after reviewing the slide show.

The presentation is divided into sections based on the genetic origin of PGE deposits: a) layered intrusions; b) flood basalt; c) komatiitic magmatism; d) greenstone belt magmatism; e) alkalic magmatism; f) orogenic magmatism and g) impact-related magmatism. These major divisions are subdivided according to the physical configuration of the mineralization Mineralization
The process by which the body uses minerals to build bone structure.

Mentioned in: Rickets

mineralization,
n the bioprecipitation of an inorganic substance.
. For example, layered intrusions are subdivided into stratiform stratiform /strat·i·form/ (-form) having a layered structure.

stratiform

occurring in layers.
 and contact deposits, with the stratiform deposits further subdivided into chromite chromite (krō`mīt), dark brown to black mineral. It is an iron-chromium oxide, FeCr2O4, with traces of magnesium and aluminum.  and sulphide-associated deposits. Each example of these topics is illustrated with one or more images, running the gamut from basic geological sketches to maps and elaborate geological block diagrams replete with geological and geochemical information. An added feature, entitled "Future exploration targets" on the CD's frontispiece but named "New opportunities" within the presentation, is appended to each of the topics. These "New opportunities" are a veritable smorgasbord of well-thought-out grassroots PGE exploration leads and ideas that may lead to discovery of new resources.

The first part, dealing with sulphide-associated PGE occurrences in layered stratiform intrusions, begins with an overview of the geology of the Muskox musk·ox or musk ox  
n. pl. musk·ox·en
A large, stocky, oxlike bovid (Ovibos moschatus) native to the coastal regions of northern Canada and Greenland, having broad flat horns with curved tips and a long, shaggy, brown or
 intrusion and its PGE concentrations, followed by descriptions of the geology, geophysics and PGE discoveries of the Fox River sill and the Mechanic intrusion in New Brunswick. The next segment, addressing stratiform PGE associated with chromite, features the geology and mineralization of Crystal Lake, the Muskox intrusion, the Bird River sill, Big Trout Lake, the Menarik intrusion and the Puddy Lake intrusion. This is followed by a segment highlighting PGE mineralization concentrated as a result of the physicochemical physicochemical /phys·i·co·chem·i·cal/ (fiz?i-ko-kem´ik-il) pertaining to both physics and chemistry.

phys·i·co·chem·i·cal
adj.
1. Relating to both physical and chemical properties.
 interaction of intrusive rocks and host rock. Examples are provided for the Muskox Intrusion, Pyrrhotite pyrrhotite (pĭr`ətīt) or magnetic pyrites, bronze-yellow to bronze-red mineral, a sulfide of iron sometimes containing nickel. It tarnishes easily and is somewhat magnetic.  Lake, the Fox River sill, the East Bull Lake, Agnew and River Valley intrusions of the Sudbury Basin and finally, the Lac des Isles Intrusion in Ontario, site of our single active Canadian mine producing exclusively PGE.

The second part deals with flood basalt magmatism and is subdivided into two segments: continental and oceanic environments. The continental environment features the massive intrusions of the midcontinental rift system, such as the Duluth gabbroic complex and associated intrusions, the Nipissing diabase diabase: see basalt.
diabase
 or dolerite

Fine- to medium-grained, dark gray to black intrusive igneous rock. Diabase is one of the dark rocks known commercially as “black granite.
, the huge Muskox Coppermine Mackenzie intrusive event and the Franklin intrusives in the Arctic. The oceanic segment, dealing with flood basalt environments, is restricted to the Wrangellia terrane ter·rane also ter·rain  
n.
1. A series of related rock formations.

2. An area having a preponderance of a particular rock or rock groups.



[Alteration of terrain.]
. Remnants of Wrangellia exposed on the western edge of the continent from Oregon to Yukon and Alaska contain PGE-bearing peridotite peridotite (pĕr'ēdō`tīt): see olivine.
peridotite

Coarse-grained, heavy, igneous rock that contains at least 10% olivine, other iron- and magnesium-rich minerals (generally pyroxenes), and not more than 10% feldspar.
 intruded into oceanic rocks, known as the Kluane belt.

The third part is devoted to PGE accumulations in komatiitic magmatism and highlights the Paleoproterozoic Circum Superior Ni Cu Fe sulphide-bearing occurrences. They range from a vast number of minor occurrences and showings to the exclusive "world class" rank of the Thompson and Raglan deposits. Slides provide glimpses of the geology and mineralization of the Thompson Nickel belt, the Fox River sill, the Cape Smith-Wakeham Bay belt and the Labrador trough. A look at the PGE potential of komatiites in the Hearne Province (including the Rankin Inlet deposit), the Ketvet Group the Prince Albert Group, form a fitting end to this vast collection.

The fourth part, on Greenstone-Gneiss Belt Magmatism, highlights a grab bag of small but high-grade PGE occurrences. A segment on gneissic gneiss  
n.
A banded or foliated metamorphic rock, usually of the same composition as granite.



[German Gneis, probably alteration of Middle High German ganeist,
 host rocks begins with the Rottenstone rot·ten·stone  
n.
A soft decomposed limestone, used in powder form as a polishing material.

Noun 1. rottenstone - a weathered and decomposed siliceous limestone; in powdered form it is used in polishing
tripoli
 deposit, continues with the Gordon-Werner Lake area and ends with the Namew Lake deposit. The second segment starts with an image of the of the La Ronge, Lynn Lake and the Flin Flon Domain.

A further part deals with PGE deposits associated with alkalic magmatism. Included are Pt placers associated with chromitite bodies in zoned Alaskan intrusions and PGE associated with sulphide, both as massive contact accumulations and in reef-type environments such as the Salt Chuck and Quetico intrusions and the Coldwell complex. The largely overlooked potential of felsic fel·sic  
adj.
Containing a group of light-colored silicate minerals that occur in igneous rocks.



[fel(dspar) + s(ilica) + -ic.
 intrusions and associated Cu-porphyry environments as PGE hosts is demonstrated with examples from the Entwine Lake Complex and Cordilleran alkalic porphyry copper deposits. Two examples of PGE mineralization associated with orogenic magmatism are illustrated by the Mechanic Intrusion in the Appalachians and the Giant Mascot in the Cordillera cor·dil·le·ra  
n.
An extensive chain of mountains or mountain ranges, especially the principal mountain system of a continent.



[Spanish, from cordilla, diminutive of cuerda, cord
.

The presentation ends with a visually appealing segment on impact-related magmatism and the Sudbury basin's PGE mineralization. Finally there is a review of future PGE exploration targets and the tools to find them.

This CD is a major compendium on PGE in Canada that is best used as a starting point for those interested in exploring for this important, useful and valuable family of elements. The insights gained may help to find additional deposits. I hope that a future updated edition of this volume is planned. In this updated edition I would suggest the inclusion of a searchable database listing the names of the occurrences. Hopefully an updated edition will also deal with the spelling gremlins that plague a number of the images in this edition.

Peter Theyer

Geological Survey

Manitoba Industry, Economic Development and Mines

360-1395 Ellice Avenue Winnipeg, Manitoba R3G 3P2

Ptheyer@gov.mb.ca
COPYRIGHT 2004 Geological Association of Canada
No portion of this article can be reproduced without the express written permission from the copyright holder.
Copyright 2004, Gale Group. All rights reserved. Gale Group is a Thomson Corporation Company.

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Article Details
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Author:Theyer, Peter
Publication:Geoscience Canada
Article Type:Book Review
Date:Jun 1, 2004
Words:1025
Previous Article:Mine Water Hydrogeology and Geochemistry.(Book Review)
Next Article:Geoscience for the needs of Canadians GAC presidential address, annual meeting St. Catharines, Ontario 12 May 2004.(Presidential Address)(Editorial)
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