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

Economic Geology; August 1961; v. 56; no. 5; p. 972-981
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 Wolfenden, E. B.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Bauxite in Sarawak

E. B. Wolfenden

Tropical weathering of various basic and intermediate igneous rocks has given rise to the bauxite deposits of western Sarawak. The pH of ground waters plays an important role in the genetic process. Some of the highest-grade material, such as the Munggu Belian deposits, has been formed from pyroxene andesite; other parent materials include gabbro, diorite, plagioclase amphibolite, and intensely altered andesitic and basaltic volcanic rocks. The bauxite consists principally of gibbsite, with varying amounts of quartz, kaolinitic clay minerals, and iron and titanium oxides.

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