Quick
Search: 		  
advanced search
 GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help 
Economic Geology Email Content Delivery
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Economic Geology; August 1986; v. 81; no. 5; p. 1196-1202
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 HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Parks, J.
Right arrow Articles by Hill, R. E. T.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Phase compositions and cryptic variation in a 2.2-km section of the Windimurra layered gabbroic intrusion, Yilgarn Block, Western Australia; a comparison with the Stillwater Complex

J. Parks, and R. E. T. Hill

CSIRO, Div. Miner. and Geochem., Wembley, West. Aust., Australia

This record provided courtesy of AGI/GeoRef.




This article has been cited by other articles:


Home page
 J PetrologyHome page
M.-F. ZHOU, P. T. ROBINSON, C. M. LESHER, R. R. KEAYS, C.-J. ZHANG, and J. MALPAS
Geochemistry, Petrogenesis and Metallogenesis of the Panzhihua Gabbroic Layered Intrusion and Associated Fe-Ti-V Oxide Deposits, Sichuan Province, SW China
J. Petrology, November 1, 2005; 46(11): 2253 - 2280.
[Abstract] [Full Text] [PDF]

Home page
 Can MineralHome page
W. D. Maier, C. Li, and S. A. De Waal
WHY ARE THERE NO MAJOR Ni Cu SULFIDE DEPOSITS IN LARGE LAYERED MAFIC-ULTRAMAFIC INTRUSIONS?
Can Mineral, April 1, 2001; 39(2): 547 - 556.
[Abstract] [Full Text] [PDF]


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