Hydrothermal Alteration in the Main Sulfide Zone at Unki Mine, Shurugwi Subchamber of the Great Dyke, Zimbabwe: Evidence from Petrography and Silicates Mineral Chemistry-Reference-Cited by-同舟云学术

Hydrothermal Alteration in the Main Sulfide Zone at Unki Mine, Shurugwi Subchamber of the Great Dyke, Zimbabwe: Evidence from Petrography and Silicates Mineral Chemistry

Published:2017-07-22 Issue:7 Volume:7 Page:127
ISSN:2075-163X
Container-title:Minerals
language:en
Short-container-title:Minerals

Author:

Chaumba Jeff

Publisher

MDPI AG

Subject

Geology,Geotechnical Engineering and Engineering Geology

Link

http://www.mdpi.com/2075-163X/7/7/127/pdf

Reference116 articles.

1. A model for the geochemistry of the platinum group elements in magmatic sulphide deposits;Campbell;Can. Mineral.,1984

2. Distribution of pd, rh, ru, jr, os, and au between sulfide and silicate metals

3. A Model for the Origin of the Platinum-Rich Sulfide Horizons in the Bushveld and Stillwater Complexes

4. Magmatic Sulfide Deposits: Geology, Geochemistry and Exploration;Naldrett,2004

5. Sulfide and platinum mineralization in the Merensky Reef: evidence from hydrous silicates and fluid inclusions

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