Description
Processes and Ore Deposits of Ultramafic-Mafic Magmas through Space and Time
Coordinators: Mondal Sisir K., Griffin William L.
Language: EnglishSubject for Processes and Ore Deposits of Ultramafic-Mafic Magmas...:
Keywords
Alaskan-type complexes; Archean; Archean greenstone belt; Boninite; Bushveld complex; China; Chromite; Chromite deposits; Craton margins; Crystal growth; Deep-seated origin; Distinct sources; Dry synthesis; Experimental methods; Exploration targeting; Fe-Ti oxides; Footprint; Global geodynamics; Hf-Nd-Sr isotopes; Komatiitic basalt; Large Igneous Provinces; Large igneous province; Liquid immiscibility; Lithogeochemistry; Lithological zoning; Lithospheric architecture; Mafic-ultramafic intrusion; Mafic-ultramafic rocks; Magma mixing; Magmatic Ni-Cu-PGE deposit; Magmatic nickel sulfides; Magmatic processes; Magmatism; Magnetite and ilmenite deposits; Mantle; Mantle plumes; Ni-Cu-PGE deposits; Ni-Cu-PGE sulfide deposits; Nickel; Noril'sk Province; Nuasahi-Sukinda; Nuggihalli; Os-S-Cu isotopes; PGE placers; PGE reef deposits; Phanerozoic; Platinum-group elements; Platinum-group minerals; Platinum-group phases; Podiform chromitites; Proterozoic; Recharge; Secular change; Silica-glass tube method; Single crystal; Stratiform chromitites; Subduction-zone magmatism; Sulfide; Sulfide horizons; Supercontinent cycle; Suprasubduction zone; Taimyr Province; Tectonic stress switches; Timing; Ultramafic-mafic intrusions; Zircon
Support: Print on demand
Description
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Processes and Ore Deposits of Ultramafic-Mafic Magmas through Space and Time focuses on the fundamental processes that control the formation of ore deposits from ultramafic-mafic magmas, covering chromite, platinum-group element (PGE), Ni-sulfides and Ti-V-bearing magnetite. The exploration, exploitation and use of these magmatic ores are important aspects of geology and directly linked to the global economy. Magmatic ores form from ultramafic-mafic magmas and crystallize at high-temperature after emplacement into crustal magma chambers, and are genetically linked to the evolution of the parental magmas through space and time. This book features recent developments in the field of magmatic ore deposits, and is an essential resource for both industry professionals and those in academia.
1. Introduction 2. Global To District Scale Controls And Signature Of Orthomagmatic Ni-Cu(-PGE) & PGE Reef Deposits 3. Exploration for the Ni-Cu-sulfide ore deposits 4. Ore deposits associated with ultramafic-mafic rocks and ore forming processes 5. Magmatic evolution of the Bushveld magma chamber: the roles of fractional crystallization, convection, magma recharge and eruption 6. Changing patterns of the mantle processes and formation of the ophiolitic chromite deposits through space and time 7. Petrogenetic evolution of the chromite deposits in the Archean greenstone belts 8. New insights on the origin of ultramafic-mafic intrusions and associated PGE-Cu-Ni sulphide deposits of the Noril’sk and Taimyr provinces, Russia: evidence from radiogenic and stable isotopes 9. Chinese ultramafic-mafic rocks and the related magmatic ore deposits 10. Alaskan-type ultramafic-mafic complexes and their magmatic ores 11. Experimental aspects of platinum-group minerals
Geologists, geochemists, exploration geologists, volcanologists, and mining and metallurgy professionals
William L. Griffin is an Honorary Professor of geology at Macquarie University in Sydney, Australia. Dr. Griffin’s research interests include the petrology and geochemistry of the deep crust and lithospheric mantle, the geochemical and dynamic evolution of the crust-mantle system, and magma generation and metasomatism in the crust and mantle. He received his PhD from the University of Minnesota.
- Elucidates the relationships between tectonic settings and magmatic ore mineralization
- Provides the links between magma generation in the mantle and ore mineralization at crustal levels
- Features the latest research on changing patterns in magmatic ore mineralization through time and their bearing on the chemical evolution of the Earth’s mantle