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

Clay Minerals; June 2007; v. 42; no. 2; p. 145-151; DOI: 10.1180/claymin.2007.042.2.01
© 2007 Mineralogical Society of Great Britain and Ireland
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 ISI 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 ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by MURRAY, H. H.
Right arrow Articles by BASTOS, C. H.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Mining, processing and applications of the Capim Basin kaolin, Brazil

H. H. MURRAY1,*, C. A. ALVES2 and C. H. BASTOS2

1 Indiana University, 1001 E. 10th St., Bloomington, IN 47405, USA, and 2 Companhia Vale do Rio Doce (CVRD), Belem, Pará, Brazil

* E-mail: murrayh{at}indiana.edu

(Received 8 November 2006; revised 31 January 2007)

High-quality kaolins are produced from two sites in the Capim River area in Pará State, northern Brazil. One mine is operated by Rio Capim Caulim (RCC) owned by Imerys and the other by Pará Pigmentos S.A. (PPSA) owned by Caemi (CVRD Group). The kaolin deposits are located on low-relief plateaux with a lateritic cap. The kaolin strata are in the Ipixuna Formation of Upper Cretaceous Age. There are two distinct kaolin layers, a 4–5 m thick soft kaolin which is overlain in the southern portion of the basin by a 4–5 m thick hard kaolin. The soft and hard designations refer to particle size, with the soft kaolin being relatively coarse and the hard kaolin very fine. The kaolin is mined, partially beneficiated, and pumped through pipelines to the port at Barcarena on the Guama River, a large tributary of the Amazon River. The PPSA kaolin is fully processed at the plant near the mine site and pumped to Barcarena where it is spray dried. The RCC kaolin is only partially processed at the mine site. This partially processed kaolin is pumped to Barcarena where it is beneficiated. The finished kaolin is high quality and is shipped to North and South American, European, and Asian paper-coating markets. More than 1.6M tons were shipped from Barcarena in 2005.

KEYWORDS: Rio Capim, kaolin, geological occurrence, paper coating, kaolin processing, Brazil




This article has been cited by other articles:


Home page
Clay MineralsHome page
R. B. SCORZELLI, L. C. BERTOLINO, A. B. LUZ, M. DUTTINE, F. A. N. G. SILVA, and P. MUNAYCO
Spectroscopic studies of kaolin from different Brazilian regions
Clay Minerals, March 1, 2008; 43(1): 129 - 135.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Mineralogical Society of Great Britain and Ireland