Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Economic Geology Don't get GSW? Talk to your librarian.
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Economic Geology; January 2002; v. 97; no. 1; p. 165-172; DOI: 10.2113/97.1.165
© 2002 Society of Economic Geologists
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 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 HighWire
Right arrow Citing Articles via Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Som, S. K.
Right arrow Articles by Joshi, R.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Scientific Communications

CHEMICAL WEATHERING OF SERPENTINITE AND Ni ENRICHMENT IN Fe OXIDE AT SUKINDA AREA, JAJPUR DISTRICT, ORISSA, INDIA

S. K. Som{dagger}

Geological Survey of India, Opn: WB-S-A&N, GSI office complex, DK block, Sector II, Salt Lake City, Kolkata-700 091, India

R. Joshi

Geological Survey of India, Zorem Building, Nongrim Hills, Shillong 793003, India

{dagger} Corresponding author: e-mail, SKSOM{at}rediffmail.com

The chromiferous serpentinite of Sukinda block of Orissa, India, has undergone extensive lateritization with secondary nickel enrichment. The vertical profile comprises partially altered serpentinite, saprolite, laterite (in situ), and laterite (transported). Mineralogical and chemical investigations reveal that nickel is released from serpentine (nepouite) by chemical weathering and has partly been residually enriched in goethite along with supergene enrichment in goethite and Mn oxides. Apparent percentage change of elements indicates that nickel is enriched in the saprolite part of the vertical column along with iron and manganese.




This article has been cited by other articles:


Home page
Clay MineralsHome page
R. Yongue-Fouateu, M. Yemefack, A. S. L. Wouatong, P. D. Ndjigui, and P. Bilong
Contrasted mineralogical composition of the laterite cover on serpentinites of Nkamouna-Kongo, southeast Cameroon
Clay Minerals, June 1, 2009; 44(2): 221 - 237.
[Abstract] [Full Text] [PDF]


Home page
Reviews in Mineralogy and GeochemistryHome page
M. A. A. Schoonen, C. A. Cohn, E. Roemer, R. Laffers, S. R. Simon, and T. O'Riordan
Mineral-Induced Formation of Reactive Oxygen Species
Reviews in Mineralogy and Geochemistry, January 1, 2006; 64(1): 179 - 221.
[Full Text] [PDF]




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