Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Economic Geology Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Economic Geology; August 2008; v. 103; no. 5; p. 1057-1077; DOI: 10.2113/gsecongeo.103.5.1057
© 2008 Society of Economic Geologists
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Sudbury Map-2pages
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Ames, D. E.
Right arrow Articles by Wodicka, N.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Geology of the Giant Sudbury Polymetallic Mining Camp, Ontario, Canada

D. E. Ames1,{dagger}, A. Davidson2 and N. Wodicka3

1 Geological Survey of Canada, 601 Booth St., Ottawa, ON K1A 0E8, Canada
2 3259 Margaret Rd., Regina, SK S4V 1B2, Canada
3 Geological Survey of Canada, 601 Booth St., Ottawa, ON K1A 0E8, Canada

{dagger} Corresponding author: e-mail, dames@NRCan.gc.ca

The first 20% of the full text of this article appears below.


    Introduction
 
A NEW, 1:100,000 SCALE compilation bedrock geology map provided with this issue presents a geologic synthesis of Canada’s most prolific mining camp, the world-class Sudbury structure with total past production and current reserves of over 1.7 billion tonnes of Ni, Cu, Co, Pt, Pd, Au, Ag ore (Lydon, 2007). The polymetallic ore is hosted within one of Earth’s largest preserved impact craters. The new map of the Ni-Cu-PGE Sudbury district (after Ames et al., 2005) is included in a pocket at the back of this issue (Map 1) and is linked to mineral deposit-commodity and geochronology data in Tables 1Go and 2Go of this paper.


View this table:



 
TABLE 1. List of Mineral Deposits and Occurrences of the Sudbury Map Area (Map 1)
 

View this table:



 
TABLE 2. U-Pb Isotope Data Across the Map Area
 
Since 1891, six compilation maps of the geology of Sudbury have been published (Bell, 1891; Collins, 1937; Cooke, 1946; Card, 1969; Dressler, 1984; Ames et al., 2005) (Fig. 1Go). Some of the Ni-Cu-PGE mines have operated for over a century, whereas new ore deposits, discovered as recently as 2004, are already in production or are in the process of being developed (i.e., advanced prospects). In the last 15 years, Sudbury has been the training ground for ~60 postgraduate geoscience students in North America (Fig. 1Go). From 1903 to 1990, only 23 graduate theses were completed on Sudbury-related topics; eight of them in the 1970s, after the discovery of shatter cones (Dietz, 1964).


Figure Removed (Available Only in the Full Text)
View larger version (19K):



 
FIG. 1. Number of graduate theses of North American geoscientists trained on Sudbury geology per decade, showing the minor peak in training after the discovery of shatter cones and the recent "education boom," with over 50 geoscience graduate theses completed since 1990. The dashed lines represent the regional geologic maps . . . [Full Text of this Article]

 






JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Society of Economic Geologists