Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Geochemistry: Exploration, Environment, Analysis Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Geochemistry: Exploration, Environment, Analysis; May 2004; v. 4; no. 2; p. 161-170; DOI: 10.1144/1467-7873/03-033
© 2004 Geological Society of London
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
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
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Garrett, R. G.
Right arrow Articles by Vutchkov, M.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Original Article

Geochemical exploration for gold in Jamaica: a comparison of stream sediment and soil surveys

Robert G. Garrett1, Gerald C. Lalor2 and Mitko Vutchkov2

1 Geological Survey of Canada, 601 Booth St., Ottawa, Ontario, Canada, K1A 0E8 (e-mail: garrett@gsc.NRCan.gc.ca)
2 International Centre for Environmental and Nuclear Sciences, University of the West Indies, Mona, Kingston 7, Jamaica (e-mail: gerald.lalor@uwimona.edu.jm and mitko@uwimona.edu.jm)

The geology of Jamaica is reviewed with reference to gold. Two geochemical surveys, one employing stream sediments for mineral exploration in selected regions of Jamaica considered a priori to have greater mineral potential, and the other an island-wide low-density soil survey to meet agro-environmental objectives, were undertaken in 1986 and 1988, respectively. The paper presents an interpretation of the previously unpublished soil data for gold, and undertakes a comparison of the two surveys in terms of their effectiveness for gold exploration. The stream sediment survey (1 site per 1 km2) led to the discovery of three new gold occurrences, one of which became a producing mine in 2001, and the recognition of two previously known auriferous districts. The low-density soil survey (1 site per 64 km2) identified the host rocks of three of these auriferous districts as having gold potential, including those of the producing mine, demonstrating its value as a broad-scale regional mineral reconnaissance tool. Geochemical studies of gold in Jamaica are complicated by the presence of transported palaeo-anomalies, related to Miocene ash-falls, in terra rossa soils in karst terrain. The Fe/Na ratio is an index of soil maturity and increases over two-and-a-half orders of magnitude with increasing soil age and mature. The plotting of Au versus the Fe/Na ratio in soils offers a simple procedure for identifying samples most likely to be related to gold occurrences in bedrock, i.e. high Au and low Fe/Na ratio. It is concluded that in the specific instance of Jamaica's high relief terrain and the apparent limitation of gold occurrences to the Cretaceous Inliers and Eocene Wagwater Trough underlying those high relief areas, stream sediment sampling is the most effective mineral exploration tool.

KEYWORDS: Caribbean, Jamaica, mineral reconnaissance, gold, exploration, soil, karst, terra rossa, palaeo-anomalies




This article has been cited by other articles:


Home page
Geochemistry: Exploration, Environment, AnalysisHome page
R. G. Garrett and G. C. Lalor
The Fe/Na ratio, a framework for modelling trace element distributions in Jamaican soils
Geochemistry: Exploration, Environment, Analysis, May 1, 2005; 5(2): 147 - 157.
[Abstract] [Full Text] [PDF]




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