Platinum group elements in mafic-ultramafic rocks of the Western Gneiss Terrain, Western Australia

1987 ◽  
Vol 36 (3-4) ◽  
pp. 247-265 ◽  
Author(s):  
M. Cornelius ◽  
E. F. Stumpfl ◽  
D. Gee ◽  
W. Prochaska
Keyword(s):  
Western Australia ◽  
Platinum Group Elements ◽  
Ultramafic Rocks ◽  
Platinum Group

Platinum-group elements in alpine-type ultramafic rocks and related chromite ores of the main ophiolite belt of the Urals

2009 ◽  
Vol 51 (2) ◽  
pp. 162-178 ◽  
Author(s):  
Yu. A. Volchenko ◽  
V. A. Koroteev ◽  
I. I. Neustroeva
Keyword(s):  
Platinum Group Elements ◽  
Ultramafic Rocks ◽  
The Urals ◽  
Ophiolite Belt ◽  
Platinum Group

Efficiency of a re-usable Carius tube for determination of platinum group elements in ultramafic rocks

2014 ◽  
Vol 33 (1) ◽  
pp. 45-52 ◽  
Author(s):  
Yingying Liu ◽  
Liang Qi ◽  
Zheng Zhao ◽  
Xiaowen Huang ◽  
Yichang Wang
Keyword(s):  
Platinum Group Elements ◽  
Ultramafic Rocks ◽  
Platinum Group

scholarly journals Different Origins of the Fractionation of Platinum-Group Elements in Raobazhai and Bixiling Mafic-Ultramafic Rocks from the Dabie Orogen, Central China

2012 ◽  
Vol 2012 ◽  
pp. 1-11 ◽  
Author(s):  
Qing Liu ◽  
Quanlin Hou ◽  
Liewen Xie ◽  
Hui Li ◽  
Shanqin Ni ◽  
...  
Keyword(s):  
Partial Melting ◽  
Fractional Crystallization ◽  
Platinum Group Elements ◽  
Central China ◽  
Assay Method ◽  
Ultramafic Rocks ◽  
Dabie Orogen ◽  
Fire Assay ◽  
Platinum Group ◽  
Different Origins

Concentrations of the platinum group elements (PGEs), including Ir, Ru, Rh, Pt, and Pd, have been determined for both Raobazhai and Bixiling mafic-ultramafic rocks from the Dabie Orogen by fire assay method. Geochemical compositions suggest that the Raobazhai mafic-ultramafic rocks represent mantle residues after variable degrees of partial melting. They show consistent PGE patterns, in which the IPGEs (i.e., Ir and Ru) are strongly enriched over the PPGEs (i.e., Pt and Pd). Both REE and PGE data of the Raobazhai mafic-ultramafic rocks suggest that they have interacted with slab-derived melts during subduction and/or exhumation. The Bixiling ultramafic rocks were produced through fractional crystallization and cumulation from magmas, which led to the fractionated PGE patterns. During fractional crystallization, Pd is in nonsulfide phases, whereas both Ir and Ru must be compatible in some mantle phases. We suggest that the PGE budgets of the ultramafic rocks could be fractionated by interaction with slab-derived melts and fractional crystallization processes.

Platinum-group elements and gold in the komatiite-hosted Fe-Ni-Cu sulfide deposits at Kambalda, Western Australia

1986 ◽  
Vol 81 (5) ◽  
pp. 1226-1235 ◽  
Author(s):  
A. Cowden ◽  
M. J. Donaldson ◽  
Anthony J. Naldrett ◽  
I. H. Campbell
Keyword(s):  
Western Australia ◽  
Platinum Group Elements ◽  
Sulfide Deposits ◽  
Platinum Group

Geochemistry of platinum group elements in mafic-ultramafic rocks of Xinjie intrusion

1999 ◽  
Vol 18 (3) ◽  
pp. 242-249
Author(s):  
Zhang Chengjiang ◽  
Wang Yunliang ◽  
Li Xiaolin ◽  
Xiu Shuzhi ◽  
Huang Yongjian
Keyword(s):  
Platinum Group Elements ◽  
Ultramafic Rocks ◽  
Platinum Group

Use of geochemistry as a guide to platinum group element potential of mafic-ultramafic rocks: examples from the west Pilbara Block and Halls Creek Mobile Zone, Western Australia

1991 ◽  
Vol 50 (1-2) ◽  
pp. 1-35 ◽  
Author(s):  
S.-S. Sun ◽  
D.A. Wallace ◽  
D.M. Hoatson ◽  
A.Y. Glikson ◽  
R.R. Keays
Keyword(s):  
Western Australia ◽  
Platinum Group Element ◽  
Group Element ◽  
Ultramafic Rocks ◽  
The West ◽  
Platinum Group

The Agnew nickel deposit, Western Australia; Part II, Sulfide geochemistry, with emphasis on the platinum-group elements

1988 ◽  
Vol 83 (3) ◽  
pp. 537-550 ◽  
Author(s):  
Stephen J. Barnes ◽  
Martin J. Gole ◽  
Robin E. T. Hill
Keyword(s):  
Western Australia ◽  
Platinum Group Elements ◽  
Nickel Deposit ◽  
Platinum Group
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