Magmatic Ni-Cu-Pge mineral lithogeochemistry I [videorecording] Download PDF EPUB FB2
Magmatic sulfide deposits fall into two major groups when considered on the basis of the value of their contained metals, one group in which Ni, and, to a lesser extent, Cu, are the most valuable products and a second in which the PGE are Magmatic Ni-Cu-Pge mineral lithogeochemistry I [videorecording] book most important.
Magmatic sulfide deposits can be subdivided into 1) Ni-Cu-PGE deposits, which have relatively smooth mantle-normalized metal patterns, 2) Ni-Cu-(PGE) deposits, which are depleted in PGE relative to Ni-Cu-Co, and 3) PGE-(Cu)-(Ni) deposits, which are enriched in PGE relative to Ni-Cu-Co.
China contains almost exclusively deposits in the second group, including the world’s Cited by: 3. magmatic Ni-Cu-PGE deposits. Tony’s students are involved in virtually every aspect of the Ni and PGE industries.
He has served as mentor to many of the authors of the chapters con-tained in this book, and his willingness and desire to share his vast knowledge of magmatic ore deposits is a mark of the educator and the gentleman that Tony by: Most major magmatic Cu-Ni-PGE sulphide deposits are thought to have formed by segregation of an immiscible sulphide melt from a silicate host magma, in response to processes such as magma mixing, rapid cooling, differentiation, and by: Baumgartner RJ, Fiorentini M, Baratoux D, Micklethwaite S, Sener AK, Lorand JP et al.
Magmatic controls on the genesis of Ni-Cu +/- (PGE) sulphide mineralisation on Mars. Ore Geology Reviews. Mar;Cited by: 8. In the mineral system approach applied to magmatic Ni-Cu-PGE sulphide deposits Barnes et al. () pointed out several criteria in targeting and evaluation. Based on.
Exploration for magmatic Ni-Cu-PGE Magmatic Ni-Cu-Pge mineral lithogeochemistry I [videorecording] book deposits: a review of recent advances in the use of geochemical tools, and their application to some South African ores W.D.
Maier Department of Geology, University of Pretoria, Pretoria, Republic of South Africa S.-J. Barnes CERM, Universite du Quebec, Chicoutimi G7H 2B 1, Canada S.A. de WaalFile Size: 1MB. Discrimination between Magmatic and Hydrothermal Ni-Cu-PGE and PGE Mineralization C.
Lesher and R.R. Keays Mineral Exploration Research Centre, Department of Earth Sciences, Laurentian University, Sudbury, ON P3E 6B5, Canada e-mail: [email protected] Introduction Mafic-ultramafic-hosted Ni-Cu-(PGE) andFile Size: KB.
Mantle-derived magmas and magmatic Ni-Cu-(PGE) deposits Excellent books on the subject of magmatic sulfide ores are available authored by Naldrett (Naldrett (. Cu-rich magmatic Ni-Cu-PGE deposits Top magmatic deposit producers () SIMEXMIN Symposium Deposit Location Operator(s) Cu pa (tonnes) Cu Grade Noril'sk Taimyr Peninsula, Russia Nori'sk Nickel% Sudbury Ontario, Canada Vale Glencore% Voisey's Bay Labrador, Canada V %File Size: 7MB.
Components of a Ni–Cu–PGE sulphide mineral system Geodynamic history and setting. The importance of tectonic setting as a targeting criterion for Ni–Cu–PGE sulphide deposits has been recognised for many decades (Naldrett,Naldrett,Naldrett, b, Naldrett, ).
A consensus had formed by the mid to late s that Cited by: than strictly magmatic. Because the focus of this paper is on Ni-Cu-(PGE) deposits, Type III deposits will not be considered in much detail. Host Rocks and Parental Magmas With the exception of the Sudbury deposits, which formed in a crustal impact melt, magmatic Ni-Cu-(PGE) deposits are hosted by a wide range of olivine-bearing mantle-derived Cited by: Lesher CM, Keays RR () Komatiite-associated Ni-Cu-(PGE) deposits.
In: Cabri LJ (ed) The Geology, Geochemistry, Mineralogy, and Mineral Beneficiation of Platinum-Group Elements. CIM Special Volume – Google ScholarCited by: 4.
The Nebo–Babel Ni–Cu–platinum-group element (PGE) sulphide deposit in the West Musgrave Block, Western Australia, is the largest nickel sulphide discovery in the last 10 years. The deposit is hosted within a concentrically zoned, olivine-free, tube-like (chonolithic), gabbronorite intrusion associated with the, approximately, 1,Ma Giles Cited by: LITHOGEOCHEMISTRY IN MINERAL EXPLORATION Pamphlet – January 1, by Ian Govett, G.J.S.
& Nichol (Author) See all formats and editions Hide other formats and editions. Price New from Used from Pamphlet, January 1, "Please retry" Author: Ian Govett, G.J.S.
& Nichol. Magmatic Ni-Cu sulfide ores may contain platinum-group elements (PGE) that are recoverable as by-products of mining these ores. It is of interest to understand which minerals host the PGE for two reasons: 1) to efficiently extract the PGE; 2) to understand the petrogenesis of the ores.
The distribution of PGE from magmatic Ni-Cu-PGE deposits at the Creighton Mine, Sudbury, Author: Sarah A. Dare, Sarah-Jane Barnes, Hazel Margaret Prichard, Peter C. Fisher. Geochemistry, geochronology, and geodynamic setting of Ni–Cu ± PGE mineral prospects hosted by mafic and ultramafic intrusions in the Portneuf–Mauricie Domain, Grenville Province, Quebec.
A.-A. Sappin, a M. Constantin, a T. Clark, b O. van Breemen cCited by: Till indicator mineral and geochemical signatures of magmatic Ni-Cu deposits, Thompson Nickel Belt M.B. McClenaghan, S.A. Averill, I.M. Kjarsgaard, D. Layton-Matthews and G. Matile Shortcourse: Drift Exploration in Manitoba Manitoba Mining.
Magmatic Ore Deposits in Layered Intrusions—Descriptive Model for Reef-Type PGE and Contact-Type Cu-Ni-PGE Deposits. Open-File Report – U.S. Department of the Interior. U.S. Geological Survey.
A review of conduit-related Ni-Cu-(PGE) sulfide mineralization at the Voiseys Bay Deposit, Labrador, and the Eagle Deposit, northern Michigan / Edward M. Ripley and Chusi Li Insights into the geologic setting and origin of Ni-Cu-PGE sulfide deposits of the Norilsk-Talnakh Region, Siberia / Nicholas T.
Arndt. Noble Metals, Subcontinental Lithosphere, and Ni-Cu-PGE Deposits Posted on by stevepiercey Recent research by Kamenetsky et al. published in Geology provides insight into the nature of the parental magmas potentially responsible for the formation of nickel-copper-platinum group element (Ni-Cu-PGE) deposits in intra-plate environments.
The Jinchuan Ni-Cu-PGE deposit is located in north-central Gansu Province, China, some km NNW of Lanzhou, and km to the west of Beijing. The Jinchuan Ni-Cu-PGE deposit (> Mt @ % Ni, % Cu, ~ g/t PGE), one of the largest magmatic sulphide deposits in the world, is located within the westernmost terrane of the North China Craton.
The integrated analysis of seismic rock properties, lithogeochemical data, and mineral compositional data, estimated via scanning electron microscopy-energy dispersive X-ray spectroscopy (SEM-EDS), provides insight into the effects of hydrothermal alteration on seismic reflectivity in the footwall of the Lalor volcanogenic massive sulfide (VMS) deposit, Manitoba, Cited by: 1.
Magmatic Ore Deposits: A number of processes that occur during cooling and crystallization of magmatic bodies can lead to the separation and concentration of minerals. 1-Pegmatites 2-Layered intrusions 3-Kimberlites Examples of Magmatic ore deposits: 1-Chromite deposits 2-Nickel ŒCopper deposits 3-Platinum group metal (PGM) depositsFile Size: 1MB.
Naldrett A J, Lightfoot P C - Ni-Cu-PGE Deposits of the Norilsk Region, Siberia: Their Formation in Conduits for Flood Basalt Volcanism: in Keays R R, Lesher C M, Lightfoot P C, Farrow C E G, (Eds), Dynamic Processes in Magmatic Ore Deposits and their Application in Mineral Exploration Geological Association of Canada, Short Course Notes.
The combined Nebo-Babel Ni-Cu-PGE deposit (Table ) consists of both disseminated and massive sulfides that are hosted within a grabbronorite magma conduit emplaced into a sulfide-free orthogenisis at Ma and off-set by a fault (Seat et al., ; Godel et al., ).
Publications de périodiques/ Journal Publications: Mansur, E.T., and Barnes, S.-J. Concentrations of Te, As, Bi, Sb and Se in the Marginal Zone of the Bushveld Complex: Evidence for crustal contamination and the nature of the magma that formed the Merensky Reef. Tectonic Settings of Magmatic Sulfide Deposits in China M.-F.
Zhou 1, X.-Y. Song, R.R. Keays2, and C.M. Lesher2 1Department of Earth Sciences, University of Hong Kong, Hong Kong, China 2Mineral Exploration Research Centre, Department of Earth Sciences, Laurentian University, Sudbury, Ontario, Canada P3E 6B5 e-mail: [email protected] by: 2.
Full Text; PDF ( K) PDF-Plus ( K) Citing articles; The role of magma injection and crystal sorting in the formation of early gabbros at the Coldwell Complex, Ontario, Canada 1.
Yong-hua Cao, a David J. Good, b Robert L. Linnen, b Iain M. Samson c a The Department of Earth Sciences, Western University, London, ON N6A 5B7, Canada; Key Cited by: 1. Another mineral with a highly interesting content of inclusion phases was represented by K-feldspar (Figure 5).
This mineral phase exclusively contained crystal inclusions, of which quartz, biotite, plagioclase, and ilmenite occurred at highest frequency.
These inclusions were mostly formed during feldspar crystallisation from the magmatic source. Mineral deposit - Mineral deposit - Magmatic cumulates: Magmatic segregation is a general term referring to any process by which one or more minerals become locally concentrated (segregated) during the cooling and crystallization of a magma.
Rocks formed as a result of magmatic segregation are called magmatic cumulates. While a magma may start as a homogeneous liquid, magmatic .hydrothermal solutions), or mineral ore formation processes are researched near and on the daylight surface (Giggenbach et al., ).
The authors of this paper showed that processes of mineral ore formation evolved in the interior of modern hydrothermal-magmatic systems of an island arc during transition from progressive toFile Size: KB.Baimazhai Ni-Cu-(PGE) deposit, Jinping County, Honghe, Yunnan, China: Ni-Cu-(PGE) sulfide deposit, hosted in a small mafic–ultramafic intrusion, which intruded Ordovician sandstone and slate.
The intrusion is concentric with lens shape, about m long, m wide.