Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Economic Geology GSW 2008 Users' Group Meeting
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Economic Geology; July 1966; v. 61; no. 4; p. 760-767
This Article
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Right arrow Order Hardcopy of Full Text via AGI/GeoRef
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Presant, E. W.
Right arrow Articles by Tupper, W. M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The distribution and nature of arsenic in the soils of the Bathurst, New Brunswick, District

E. W. Presant, and W. M. Tupper

Over unmineralized bedrock, the B 1 soil horizon has the highest mean (22 ppm) and widest range (0-70 ppm) of arsenic values. 'The arsenic contents of the B and C horizons (up to 3500 ppm As above sulfide deposits) give a more reliable measure of nearby sulfide mineralization than those of the As horizons.' Beudantite was identified in coatings on soil grains in the upper B horizons. Much of the arsenic is apparently associated with iron oxides, probably in an absorbed form.

This record provided courtesy of AGI/GeoRef.







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Society of Economic Geologists