An oxygen isotope study of the Lower Mafic Succession of the Darwendale Subchamber of the Great Dyke, Zimbabwe
Author:
Publisher
Elsevier BV
Subject
Geochemistry and Petrology,Geology
Reference48 articles.
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4. Investigations of the Stillwater Complex, IV. The role of volatiles in the petrogenesis of the J-M Reef, Minneapolis Adit Section;Boudreau;Can. Mineral.,1988
5. Halogen geochemistry of the Stillwater and Bushveld Complexes: evidence for transport of the platinum-group elements by Cl-rich fluids;Boudreau;J. Petrol.,1986
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2. Petrographic and mineral chemistry evidence for the origin of sulfide mineralization in the Main Sulfide Zone, Sebakwe Subchamber of the Great Dike, Zimbabwe;Precambrian Research;2022-02
3. Geochemistry of the chromitite stringer at the contact of the mafic sequence and the ultramafic sequence in the Unki Mine area, Shurugwi Subchamber of the Great Dyke, Zimbabwe;The Canadian Mineralogist;2020-05-01
4. Mixing and Unmixing in the Bushveld Complex Magma Chamber;Processes and Ore Deposits of Ultramafic-Mafic Magmas through Space and Time;2018
5. Hydrothermal Alteration in the Main Sulfide Zone at Unki Mine, Shurugwi Subchamber of the Great Dyke, Zimbabwe: Evidence from Petrography and Silicates Mineral Chemistry;Minerals;2017-07-22
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