scholarly journals System scale and deposit scale controls on Ni-Cu-PGE mineralisation in cratonic areas and their margins

2017 ◽  
Author(s):  
W Bleeker ◽  
D E Ames
Keyword(s):  
Pge Mineralisation

Chromite and Sulphide Hosted PGE Mineralisation in Sittampundi Layered Anorthosite Complex, Tamil Nadu

2015 ◽  
Author(s):  
S. Dhanendran ◽  
N. P. Nathan ◽  
R. Vijay Kumar ◽  
Laya M. B. Pillai ◽  
A. Balukkarasu
Keyword(s):  
Tamil Nadu ◽  
Anorthosite Complex ◽  
Pge Mineralisation

Platinum group element (PGE) mineralisation and chromite geochemistry in the Berit ophiolite (Elbistan/Kahramanmaraş), SE Turkey

2014 ◽  
Vol 60 ◽  
pp. 97-111 ◽  
Author(s):  
Hatice Kozlu ◽  
Hazel Prichard ◽  
Frank Melcher ◽  
Peter Fisher ◽  
Christopher Brough ◽  
...  
Keyword(s):  
Platinum Group Element ◽  
Group Element ◽  
Platinum Group ◽  
Se Turkey ◽  
Pge Mineralisation

Shale-hosted Ni–(Cu–PGE) mineralisation: a global overview

2011 ◽  
Vol 120 (4) ◽  
pp. 187-197 ◽  
Author(s):  
S M Jowitt ◽  
R R Keays
Keyword(s):  
Pge Mineralisation

scholarly journals Cu-Ni-PGE mineralisation at the Aurora Project and potential for a new PGE province in the Northern Bushveld Main Zone

2017 ◽  
Vol 80 ◽  
pp. 1135-1159 ◽  
Author(s):  
Iain McDonald ◽  
R.E. (Jock) Harmer ◽  
David A. Holwell ◽  
Hannah S.R. Hughes ◽  
Adrian J. Boyce
Keyword(s):  
Main Zone ◽  
Pge Mineralisation

Platinum-group minerals in the Selukwe Subchamber, Great Dyke, Zimbabwe: implications for PGE collection mechanisms and post-formational redistribution

1993 ◽  
Vol 57 (389) ◽  
pp. 613-633 ◽  
Author(s):  
Bronwen M. Coghill ◽  
Allan H. Wilson
Keyword(s):  
Base Metal ◽  
Process Model ◽  
Intermediate Compound ◽  
Compound Formation ◽  
Great Dyke ◽  
Platinum Group Minerals ◽  
Single Process ◽  
Base Metal Sulphides ◽  
Platinum Group ◽  
Pge Mineralisation

AbstractThis paper presents the results of microprobe investigations of the Platinum-Group Elements (PGE) of the Selukwe Subchamber, Great Dyke, Zimbabwe. The PGE are associated with base metal sulphides in the uppermost pyroxenites of the Ultramafic Sequence of the Great Dyke. The following minerals have been indentified: bismuthotellurides (moncheite, maslovite, michenerite, kotulskite and polarite); arsenides (sperrylite); and sulphides and sulpharsenides (cooperite, laurite, braggite and hollingworthite). Platinum Group Minerals (PGM) occur in three distinct textural environments: (1) at the boundary of sulphides and silicates/hydrosilicates, (2) entirely enclosed within sulphides, and (3) entirely enclosed within silicate or hydrosilicate minerals. The stratigraphic distribution, environments and textures of the PGM have important genetic implications, and cannot be explained by a single process. A multi-process model for the petrogenesis of the PGE mineralisation in terms of complexation and intermediate compound formation is proposed. The primary mineralising events were due to orthomagmatic processes, but the observed textures are the result of microscale remobilisation of PGM components by trapped interstitial fluids (bydromagmatic processes).

Occurrence of PGE mineralisation in Bangur, Kendujhar district, Odisha

2014 ◽  
Vol 83 (1) ◽  
pp. 31-37 ◽  
Author(s):  
K. C. Sahoo ◽  
M. Mohanty ◽  
P. Sahoo ◽  
S. C. Rath ◽  
S. B. Ray
Keyword(s):  
Pge Mineralisation
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