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International Geology Review, Vol. 49, 2007, p. 169192. Copyright 2007 by V. H. Winston & Son, Inc. All rights reserved.
 

Summary: 169
International Geology Review, Vol. 49, 2007, p. 169­192.
Copyright © 2007 by V. H. Winston & Son, Inc. All rights reserved.
0020-6814/07/919/169-24 $25.00
Platinum-Group Element, Stable Isotope, and Fluid Inclusion
Investigation of the Ultramafic Rock­Hosted Gunes-Sogucak
Ni-Cu-Sulfide Mineralization in the Gunes Ophiolite,
East-Central Turkey
ALI UCURUM,1
Department of Geological Engineering, Cumhuriyet University, Sivas 58140, Turkey
PAUL J. LECHLER,
Nevada Bureau of Mines and Geology, University of Nevada Reno, Reno, Nevada 89557-0088
GREG B. AREHART,
Department of Geological Sciences, MS-172, University of Nevada Reno, Reno, Nevada 89557-0138
AND FERENC MOLNAR
Department of Mineralogy, Eötvös Loránd University, Pázmány Péter sétány 1/C, Budapest, H-1117, Hungary
Abstract
Gunes-Sogucak Ni-Cu-sulfide mineralization in the Divrigi district of Sivas Province is geneti-
cally related to Late Cretaceous ultramafic rocks. Disseminated mineralization is scattered through
the ultramafic rocks, whereas vein-type mineralization is present in fracture zones in them. Both

  

Source: Arehart, Greg B. - Department of Geological Sciences, Mackay School of Mines, University of Nevada, Reno

 

Collections: Geosciences