A garnierite with a high nickel content from Western Australia

1975 ◽  
Vol 40 (309) ◽  
pp. 65-69 ◽  
Author(s):  
E. H. Nickel ◽  
P. J. Bridge

SummaryThe garnierite, which occurs in the oxide zone overlying a nickel sulphide deposit, consists of talc-like and serpentine-like components, with the former predominating. Chemical and electron-probe analyses give NiO contents ranging between 39.6 and 43.9 weight %.

1987 ◽  
Vol 62 (3) ◽  
pp. 194-203 ◽  
Author(s):  
V. F. Vinokurov ◽  
I. V. Gorynin ◽  
G. T. Zhdan ◽  
Sh. Sh. Ibragimov ◽  
O. A. Kozhevnikov ◽  
...  

2000 ◽  
Vol 31 (1-2) ◽  
pp. 201-209 ◽  
Author(s):  
Bruce Craven ◽  
Tony Rovira ◽  
Terry Grammer ◽  
Mark Styles

1983 ◽  
Vol 47 (345) ◽  
pp. 501-505 ◽  
Author(s):  
R. van de Vusse ◽  
Roger Powell

AbstractThe ultramafic-hosted disseminated nickel sulphide deposit at Mount Keith, Western Australia, originally consisted of sulphide droplets and chrome spinels interstitial to olivine. During cooling, the sulphide droplets crystallized to pentlandite-pyrrhotine. Hydration and carbonation caused rimming and replacement of pentlandite-pyrrhotine by tochilinite, magnetite, and magnesite. These textures are interpreted in terms of diffusion between serpentinite matrix and the sulphide blebs.


1998 ◽  
Vol 29 (3-4) ◽  
pp. 273-279
Author(s):  
William J. Amann ◽  
Risto Pietila

1994 ◽  
Vol 62 (1) ◽  
pp. 48-55
Author(s):  
Hiroya YAMASHITA ◽  
Takeshi YAMAMURA ◽  
Katsutoshi YOSHIMOTO

2007 ◽  
Vol 33 (6) ◽  
pp. 313-318 ◽  
Author(s):  
Minoru HATATE ◽  
Toshio SHIOTA ◽  
Yoichi NAGASAKI ◽  
Nobuyuki ABE ◽  
Masaharu AMANO ◽  
...  

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