Relevant bibliographies by topics / Ni-Cu-PGE deposits

Academic literature on the topic 'Ni-Cu-PGE deposits'

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Published: 4 June 2021
Last updated: 6 February 2022

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Journal articles on the topic "Ni-Cu-PGE deposits"

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Moilanen, M., E. Hanski, J. Konnunaho, T. Törmänen, S. H. Yang, Y. Lahaye, H. O’Brien, and J. Illikainen. "Composition of iron oxides in Archean and Paleoproterozoic mafic-ultramafic hosted Ni-Cu-PGE deposits in northern Fennoscandia: application to mineral exploration." Mineralium Deposita 55, no. 8 (January 11, 2020): 1515–34. http://dx.doi.org/10.1007/s00126-020-00953-1.

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Abstract Using electron probe microanalyzer (EPMA) and laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS), we analyzed major and trace element compositions of iron oxides from Ni-Cu-PGE sulfide deposits hosted by mafic-ultramafic rocks in northern Fennoscandia, mostly focusing on Finland. The main research targets were the Archean Ruossakero Ni-(Cu) deposit; Tulppio dunite and related Ni-PGE mineralization; Hietaharju, Vaara, and Tainiovaara Ni-(Cu-PGE) deposits; and Paleoproterozoic Lomalampi PGE-(Ni-Cu) deposit. In addition, some reference samples from the Pechenga (Russia), Jinchuan (China), and Kevitsa (Finland) Ni-Cu-PGE sulfide deposits, and a barren komatiite sequence in the Kovero area (Finland) were studied. Magnetite and Cr-magnetite show a wide range of trace element compositions as a result of the variation of silicate and sulfide melt compositions and their post-magmatic modification history. Most importantly, the Ni content in oxide shows a positive correlation with the Ni tenor of the sulfide phase in equilibrium with magnetite, regardless of whether the sulfide assemblage is magmatic or post-magmatic in origin. The massive sulfide samples contain an oxide phase varying in composition from Cr-magnetite to magnetite, indicating that Cr-magnetite can crystallize directly from sulfide liquid. The Mg concentration of magnetites in massive sulfide samples is lowest among the samples analyzed, and this can be regarded as a diagnostic feature of an oxide phase crystallized together with primitive Fe-rich MSS (monosulfide solid solution). Our results show that magnetite geochemistry, plotted in appropriate discrimination diagrams, together with petrographical observations could be used as an indicator of potential Ni-(Cu-PGE) mineralization.
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Lu, Yiguan, C. Michael Lesher, and Jun Deng. "Geochemistry and genesis of magmatic Ni-Cu-(PGE) and PGE-(Cu)-(Ni) deposits in China." Ore Geology Reviews 107 (April 2019): 863–87. http://dx.doi.org/10.1016/j.oregeorev.2019.03.024.

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Lesher, C. M., and P. C. Lightfoot. "Preface for thematic issue on Ni–Cu–PGE deposits." Mineralium Deposita 47, no. 1-2 (August 5, 2011): 1–2. http://dx.doi.org/10.1007/s00126-011-0379-y.

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Makkonen, Hannu V., Tapio Halkoaho, Jukka Konnunaho, Kalevi Rasilainen, Asko Kontinen, and Pasi Eilu. "Ni-(Cu-PGE) deposits in Finland – Geology and exploration potential." Ore Geology Reviews 90 (November 2017): 667–96. http://dx.doi.org/10.1016/j.oregeorev.2017.06.008.

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Song, Xieyan. "Magmatic Ni-Cu and PGE Deposits: Geology, Geochemistry, and Genesis." Geoscience Frontiers 3, no. 6 (November 2012): 945. http://dx.doi.org/10.1016/j.gsf.2012.05.002.

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Hall, M. F., B. Lafrance, and H. L. Gibson. "Emplacement of sharp-walled sulfide veins during the formation and reactivation of impact-related structures at the Broken Hammer Mine, Sudbury, Ontario." Canadian Journal of Earth Sciences 57, no. 10 (October 2020): 1149–66. http://dx.doi.org/10.1139/cjes-2019-0229.

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Broken Hammer is a hybrid Cu–Ni–Platinum Group Element (PGE) footwall deposit located in Archean basement rocks below the impact-induced Sudbury Igneous Complex (SIC), Canada. The deposit consists of massive chalcopyrite veins surrounded by thin epidote, actinolite, and quartz selvedges and low-sulfide, high-PGE mineralization consisting of disseminated chalcopyrite (<5%) and platinum group minerals, associated with Ni-bearing chlorite overprinting alteration patches of epidote, actinolite, and quartz. The veins are grouped into five steeply-dipping sets, striking northeast-, southwest-, southeast-, south-, and east–west, which were emplaced along impact-related fractures that were reactivated multiple times during stabilization of the crater floor. Early reactivation of the fractures created pathways for the migration of hydrothermal fluids from which quartz and chlorite precipitated sealing the fractures. Renewed slip shattered the quartz–chlorite veins into fragments that were incorporated in massive sulfide veins that crystallized from fractionated sulfide melts or from high temperature (400–500 °C) hydrothermal fluids, which migrated outward into the basement rocks from a cooling and crystallizing SIC melt sheet. Hydrothermal fluids syn-genetic with the epidote–actinolite–quartz alteration distributed the PGE into the footwall rocks, or late hydrothermal fluids associated with the Ni-bearing chlorite leached Ni and PGMs from the sulfide veins and redistributed them to form low-sulfide, high-PGE zones in the footwall rocks. During post-impact tectonic events, slip at temperatures below the brittle–ductile transition for chalcopyrite (<200 °C to 250 °C) produced striations along the vein margins. The Broken Hammer deposit exemplifies how Cu–Ni–PGE footwall deposits formed by the reactivation of impact-related fractures that provided conduits for the migration of melts and hydrothermal fluids.
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Sluzhenikin, Sergey F., and Andrey V. Mokhov. "Gold and silver in PGE–Cu–Ni and PGE ores of the Noril’sk deposits, Russia." Mineralium Deposita 50, no. 4 (August 19, 2014): 465–92. http://dx.doi.org/10.1007/s00126-014-0543-2.

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Duran, Charley J., Sarah-Jane Barnes, Eduardo T. Mansur, Sarah A. S. Dare, L. Paul Bédard, and Sergey F. Sluzhenikin. "Magnetite Chemistry by LA-ICP-MS Records Sulfide Fractional Crystallization in Massive Nickel-Copper-Platinum Group Element Ores from the Norilsk-Talnakh Mining District (Siberia, Russia): Implications for Trace Element Partitioning into Magnetite." Economic Geology 115, no. 6 (September 1, 2020): 1245–66. http://dx.doi.org/10.5382/econgeo.4742.

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Abstract Mineralogical and chemical zonations observed in massive sulfide ores from Ni-Cu-platinum group element (PGE) deposits are commonly ascribed to the fractional crystallization of monosulfide solid solution (MSS) and intermediate solid solution (ISS) from sulfide liquid. Recent studies of classic examples of zoned orebodies at Sudbury and Voisey’s Bay (Canada) demonstrated that the chemistry of magnetite crystallized from sulfide liquid was varying in response to sulfide fractional crystallization. Other classic examples of zoned Ni-Cu-PGE sulfide deposits occur in the Norilsk-Talnakh mining district (Russia), yet magnetite in these orebodies has received little attention. In this contribution, we document the chemistry of magnetite in samples from Norilsk-Talnakh, spanning the classic range of sulfide composition, from Cu poor (MSS) to Cu rich (ISS). Based on textural features and mineral associations, four types of magnetite with distinct chemical composition are identified: (1) MSS magnetite, (2) ISS magnetite, (3) reactional magnetite (at the sulfide-silicate interface), and (4) hydrothermal magnetite (resulting from sulfide-fluid interaction). Compositional variability in lithophile and chalcophile elements records sulfide fractional crystallization across MSS and ISS magnetites and sulfide interaction with silicate minerals (reactional magnetite) and fluids (hydrothermal magnetite). Estimated partition coefficients for magnetite in sulfide systems are unlike those in silicate systems. In sulfide systems, all lithophile elements are compatible and chalcophile elements tend to be incompatible with magnetite, but in silicate systems some lithophile elements are incompatible and chalcophile elements are compatible with magnetite. Finally, comparison with magnetite data from other Ni-Cu-PGE sulfide deposits pinpoints that the nature of parental silicate magma, degree of sulfide evolution, cocrystallizing phases, and alteration conditions influence magnetite composition.
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Begg, G. C., J. A. M. Hronsky, N. T. Arndt, W. L. Griffin, S. Y. O'Reilly, and N. Hayward. "Lithospheric, Cratonic, and Geodynamic Setting of Ni-Cu-PGE Sulfide Deposits." Economic Geology 105, no. 6 (September 1, 2010): 1057–70. http://dx.doi.org/10.2113/econgeo.105.6.1057.

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Yakubchuk, Alexander, and Anatoly Nikishin. "Noril?sk?Talnakh Cu?Ni?PGE deposits: a revised tectonic model." Mineralium Deposita 39, no. 2 (March 1, 2004): 125–42. http://dx.doi.org/10.1007/s00126-003-0373-0.

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Dissertations / Theses on the topic "Ni-Cu-PGE deposits"

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Manor, Matthew John. "Convergent margin Ni-Cu-PGE deposits : geology, geochronology, and geochemistry of the Giant Mascot magmatic sulphide deposit, Hope, British Columbia." Thesis, University of British Columbia, 2014. http://hdl.handle.net/2429/51751.

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The Giant Mascot Ni-Cu-PGE deposit remains British Columbia’s only past-producing nickel mine (1958-1974) with ~4.2 Mt of ore grading 0.77% Ni, 0.34% Cu, minor Co, Ag, and Au, and unreported platinum group elements (PGE). The deposit is part of a new class of ‘convergent margin’ Ni-Cu-PGE sulphide deposits containing orthopyroxene and magmatic hornblende. The ultramafic-mafic intrusions that host these deposits have relatively small footprints, generally less than ~10 km2 (e.g., Portneuf-Mauricie Domain, Québec; Huangshandong, China; Aguablanca, Spain), and they are becoming increasingly important economic resources globally. Zircon was successfully separated from feldspathic ultramafic rocks and yield a weighted ²⁰⁶Pb/²³⁸U age of crystallization for the Giant Mascot ultramafic intrusion of ca. 93 Ma (CA-TIMS, n=8), thus constraining the age of mineralization and distinguishing it as one of the world’s youngest Ni deposits. The Giant Mascot intrusion is a crudely elliptical, 4×3 km plug composed of ultramafic arc cumulates (olivine-orthopyroxene, hornblende-clinopyroxene) that intruded the Late Cretaceous Spuzzum pluton. Sub-vertical pipe-like, lensoid and tabular bodies (n=28) host orthomagmatic Ni-Cu-PGE mineralization as disseminated, net-textured, semi-massive, and massive ores consisting of pyrrhotite, pentlandite, chalcopyrite, minor pyrite, troilite, and Pt-Pd-Ni bismuthotellurides. The sulphides have high tenors (3-14 wt% Ni, 0.1-17.1 wt% Cu, 84 ppb-5 ppm total PGE) and distinct iridium-group PGE concentrations that represent varying stages of monosulphide solid solution fractionation and subsequent metal enrichment of two magma types forming the Western and Eastern mineralized zones. Sulphur isotopes (n=34) for sulphides in ultramafic rocks reveal δ³⁴S values (-3.4 to -1.3‰) lighter than typical mantle values and overlap with analyses from locally pyritiferous Settler schist (-5.4 to -1.2‰). Sulphide saturation in the Giant Mascot parental magma(s) was triggered in response to 1) reduction of an oxidized, mantle-derived arc magma, 2) addition of external sulphur and silica by assimilation of Settler schist and Spuzzum diorites, and 4) fractional crystallization. The presence of high-tenor sulphides indicates that orogenic Ni-Cu-PGE deposits may be of greater significance to future exploration globally than previously assumed.
Science, Faculty of
Earth, Ocean and Atmospheric Sciences, Department of
Graduate
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Seat, Zoran. "Geology, petrology, mineral and whole-rock chemistry, stable and radiogenic isotope systematics and Ni-Cu-PGE mineralisation of the Nebo-Babel intrusion, West Musgrave, Western Australia." University of Western Australia. School of Earth and Geographical Sciences, 2008. http://theses.library.uwa.edu.au/adt-WU2008.0202.

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The Nebo-Babel Ni-Cu-platinum-group element (PGE) magmatic sulphide deposit, a world-class ore body, is hosted in low-MgO, tube-like (chonolithic) gabbronorite intrusion in the West Musgrave Block, Western Australia. The Nebo-Babel deposit is the first significant discovery of a nickel sulphide deposit associated with the ca. 1078 Ma Giles Complex, which is part of the Warakurna large igneous province (LIP), now making the Musgrave Block a prime target for nickel sulphide exploration. The Musgrave Block is a Mesoproterozoic, east-west trending, orogenic belt in central Australia consisting of amphibolite and granulite facies basement gneisses with predominantly igneous protoliths. The basement lithologies have been intruded by mafic-ultramafic and felsic rocks; multiply deformed and metamorphosed between 1600 Ma and 500 Ma. The Giles Complex, which is part of the Warakurna LIP, was emplaced at ca. 1078 Ma and consists of a suite of layered mafic-ultramafic intrusions, mafic and felsic dykes and temporally associated volcanic rocks and granites. The Giles Complex intrusions are interpreted to have crystallised at crustal depths between 15km and 30km and are generally undeformed and unmetamorphosed.
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Mukwakwami, Joshua. "Structural controls of Ni-Cu-PGE ores and mobilization of metals at the Garson Mine, Sudbury." Thesis, Laurentian University of Sudbury, 2013. https://zone.biblio.laurentian.ca/dspace/handle/10219/2029.

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The Garson Ni-Cu-PGE deposit is located on the South Range of the 1850 Ma Sudbury structure along the contact between the Sudbury Igneous Complex (SIC) and the underlying metasedimentary and metavolcanic rocks of the Paleoproterozoic Huronian Supergroup. It comprises four ore bodies that are hosted by E-W-trending shear zones that dip steeply to the south. The shear zones formed as south-directed D1 thrusts in response to flexural-slip during regional buckling of the SIC. They imbricated the ore zones, the SIC norite, the underlying Huronian rocks and they emplaced slivers of Huronian rocks and anatectic breccia into the overlying Main Mass norite. Coexisting garnet-amphibole pairs yielded syn-D1 amphibolite facies metamorphic temperatures ranging from ~550°C to 590°C. The shear zones were coeval with the moderately southdipping South Range and Thayer Lindsley shear zones, which formed to accommodate the strain in the hinge zone as the SIC tightened with progressive D1 shortening. The SE limb of the SIC was overturned together with the D1 thrusts, which were then reactivated as steeply south-dipping reverse shear zones during syn-D2 greenschist metamorphism. Syn-D2 metamorphic titanite yield a U-Pb age of ca. 1849 ± 6 Ma, suggesting that D1 and D2 are part of a single progressive deformation event that occurred immediately after crystallization of the SIC during the Penokean Orogeny. The ore bodies plunge steeply to the south parallel to the colinear L1 and L2 stretching mineral lineations. Ore types consist mainly of pyrrhotite-pentlandite-chalcopyrite breccia ores, but also include pyrrhotite-pentlandite-chalcopyrite disseminated sulfide mineralization in norite, and syn-D2 quartz-calcite-chalcopyrite-pyrrhotite-pentlandite iv veins. In the breccia ores, matrix sulfides surround silicate rock fragments that have a strong shape-preferred orientation defining a pervasive foliation. The fragments are highly stretched parallel to the mineral lineations in wall rocks, suggesting that the ore bodies are zones of high strain. Pyrrhotite and chalcopyrite occur in piercement structures, in boudin necks between fragments, in fractures in wall rocks and in fold hinges, suggesting that the sulfides were mobilized by ductile plastic flow. Despite evidence of high strain in the ore zones, the sulfide matrix in D1 and D2 breccia ores show little evidence of strain as they consist predominantly of polygonal pyrrhotite aggregates, suggesting that they recrystallized during, or immediately after D1 and D2. However, rare elongate pyrrhotite grains aligned parallel to S2 are locally preserved only in D2 breccia ores. Exsolution of pentlandite loops along grain boundaries of elongate pyrrhotite formed S2-parallel pentlandite-rich layers in D2 breccia ores, whereas the pentlandite loops are multi-oriented in D1 contact breccia as they were exsolved along grain boundaries polygonal pyrrhotite. Because exsolution of pentlandite post-date D1 and D2, and that individual pentlandite grains neither have a shape-preferred orientation nor show evidence for cataclastic flow, the sulfides reverted to, and were mobilized as a homogeneous metamorphic monosulfide solid solution (mss) during D1 and possibly D2. This is in agreement with predictions from phase equilibria as the average Garson composition plots within the mss field in Fe-Ni-S ternary diagram at temperatures above ~400°C. Disseminated and breccia ores at Garson have similar mantle-normalized multi-element chalcophile patterns as undeformed contact-type disseminated and massive ore, v respectively, at the well known Creighton mine in the South Range. This suggests that the Garson ores are magmatic in origin and that their compositions were not significantly altered by hydrothermal fluids and deformation. The lack of variations in Ni tenors between the disseminated and breccias ores suggest that the R-factor was not the process controlling metal tenors because the disseminated sulfides do not consistently have higher metal tenors than the breccia ore. The breccia ores are enriched in Rh-Ru-Ir and are depleted in Cu-Pd-Pt-Au, in contrast to footwall-type ore at the nearby Garson Ramp mine which is enriched in the same metals. When Ni100, Rh100, Ir100, Pt100 and Pd100 are plotted against Cu100, the breccia and footwall-type ore analyses plot along model mss fractionation and sulfide melt model curves, suggesting that these two ore types are related by mss fractionation. In summary, the Garson breccia ores are mss cumulates that settled quickly at the base of the SIC via a gravity filtration process, and were mobilized as a metamorphic mss by ductile plastic flow during D1 and D2. Despite minor local hydrothermal mobilization of some metals, the study confirms findings from other studies that highly deformed Ni-Cu- PGE deposits, such as the Garson deposit, can provide important information on the genesis of the deposits.
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Brownscombe, William. "The geology and geochemistry of the Sakatti Cu-Ni-PGE deposit, N. Finland." Thesis, Imperial College London, 2015. http://hdl.handle.net/10044/1/61898.

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The Sakatti Cu-Ni-PGE (platinum group elements) deposit is a newly discovered mineral deposit in northern Finland. The deposit is a magmatic sulphide hosted in an ultramafic intrusion in the Central Lapland Greenstone Belt. The major lithologies and styles of mineralisation of the deposit are characterised and defined in this project and their origin investigated. The host rock is composed primarily of olivine with forsterite content between 0.85 and 0.91 and a Ni content between 3000-3700 ppm. This suggests that the olivine is undepleted with respect to Ni and has not been derived from a sulphide-saturated melt. The intrusion sits in a plagioclase-picrite and the locus of the deposit occurs at a change in gradient that occurs when the intrusion transgresses to a stratigraphically higher lithology. Sulphur isotope analysis shows that the Sakatti deposit has consistent δ34S values 2.6 ± 2.4 ‰. This is not consistent with the regional Matarakoski schists contributing S to the deposit. The deposit has unusually low Ni/Cu values, particularly the shallower portions. Magnetite trace element analysis, PPGE/IPGE values and Ni isotope analysis presented suggest that this is due to sulphide fractionation and loss of early fractionating Ni-rich sulphide cumulates. The PGE mineralogy in the Sakatti deposit is exclusively PGE tellurides, derived from sulphide melt. The dominance of tellurides leads to a wide array of moncheite-merenskyite-melonite compositions that is not seen elsewhere globally. A model is presented for the formation of the deposit where earlier Ni-rich cumulates are lost at an earlier stage in the conduit-like intrusion and remobilised by later silicate melt that does not re-equilibrate with the sulphides.
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Kormos, Steven. "Metal distribution within Zone 39, a Proterozoic vein-type Cu-Ni-Au-Ag-PGE deposit, Strathcona Mine, Ontario, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0027/MQ46486.pdf.

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Hanley, Jacob James. "Experimental and fluid inclusion constraints on the ore metal content and origin of volatiles associated with large NI-CU--PGE deposits /." 2006. http://link.library.utoronto.ca/eir/EIRdetail.cfm?Resources__ID=442629&T=F.

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Books on the topic "Ni-Cu-PGE deposits"

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Piña, Rubén. The Ni-Cu-(PGE) Aguablanca Ore Deposit (SW Spain). Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-93154-8.

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Huminicki, Michelle A. E. Geology, mineralogy, and geochemistry of the Kelly Lake Ni-Cu-PGE deposit, Sudbury, Ontario. Sudbury, Ont: Laurentian University, School of Graduate Studies, 2002.

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Kormos, Steven E. Metal distribution within zone 39, a proterozoic vein-type Cu-Ni-Au-Ag-PGE deposit, Strathcona Mine, Ontario, Canada. Sudbury, Ont: Laurentian University, Department of Earth Sciences, 1999.

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Gregory, Steven Kelvey. Geology, mineralogy, and geochemistry of transitional contact/footwall mineralization in the McCreedy East NI-CU-PGE deposit, Sudbury igneous complex. Sudbury, Ont: Laurentian University, School of Graduate Studies, 2005.

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Chisholm, Kevin Malcolm. Nature and origin of ore-localizing embayments at the Katinniq Ni-Cu-(PGE) sulphide deposit, Cape Smith Belt, Northern Quebec. Sudbury, Ont: Laurentian University, Department of Earth Sciences, 2002.

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John, Fedorowich, Morrison Gord, Geological Association of Canada, and Minerological Association of Canada, eds. Sudbury NI-CU-PGE deposits: South Sange (A-1) and North Range (B-1) : field trips A1 & B1 guidebooks. Sudbury, Ont: Geological Association of Canada, 1999.

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John, Fedorowich, Morrison Gord, Geological Association of Canada, and Minerological Association of Canada, eds. Sudbury NI-CU-PGE deposits: South Sange (A-1) and North Range (B-1) : field trips A1 & B1 guidebooks. Sudbury, Ontario: Geological Association of Canada, 1999.

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Hanley, Jacob James. Experimental and fluid inclusion constraints on the ore metal content and origin of volatiles associated with large NI-CU--PGE deposits. 2006.

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Book chapters on the topic "Ni-Cu-PGE deposits"

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Piña, Rubén. "The Aguablanca Ni–Cu–(PGE) Sulfide Deposit." In SpringerBriefs in World Mineral Deposits, 31–57. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-93154-8_4.

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Wenyuan, Li, Wang Wei, and Guo Zhouping. "Magmatic Ni-Cu-PGE deposits in the Qilian-Longshou mountains, Northwest China — part of a Proterozoic large igneous province." In Mineral Deposit Research: Meeting the Global Challenge, 429–31. Berlin, Heidelberg: Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_112.

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Kislov, E. V. "Ni-Cu-PGE mineralization in the Upper Proterozoic loko-Dovyren mafic-ultramafic massif, Russia." In Mineral Deposit Research: Meeting the Global Challenge, 413–16. Berlin, Heidelberg: Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_108.

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Pirajno, Franco, and Paul Morris. "Large igneous provinces in Western Australia: Implications for Ni-Cu and Platinum Group Elements (PGE) mineralization." In Mineral Deposit Research: Meeting the Global Challenge, 1049–52. Berlin, Heidelberg: Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_268.

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Paniagua, A., I. Fanlo, B. Garcia, I. Subias, F. Gervilla, and R. D. Acevedo. "Unusual PGE concentration in early disulfides of a low-temperature hydrothermal Cu-Ni-Co-Au deposit at Villamanin (Leon, northern Spain)." In Mineral Deposit Research: Meeting the Global Challenge, 1033–36. Berlin, Heidelberg: Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_264.

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Ripley, E. M., C. Li, and J. Thakurta. "Magmatic Cu-Ni-PGE mineralization at a convergent plate boundary: Preliminary mineralogic and isotopic studies of the Duke Island Complex, Alaska." In Mineral Deposit Research: Meeting the Global Challenge, 49–51. Berlin, Heidelberg: Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_13.

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Krivolutskaya, Nadezhda, Maria Nesterenko, Bronislav Gongalsky, Dmitry Korshunov, Yana Bychkova, and Natalia Svirskaya. "Unique PGE-Cu-Ni Oktyabr’skoe Deposit (Noril’sk Area, Siberia, Russia): New Data on Its Structure and Mineralization." In Petrogenesis and Exploration of the Earth’s Interior, 253–55. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01575-6_61.

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Jesus, Ana P., António Mateus, José Munhá, and Álvaro Pinto. "Intercummulus massive Ni-Cu-Co and PGE-bearing sulphides in pyroxenite: a new mineralization type in the layered gabbroic sequence of the Beja Igneous Complex (Portugal)." In Mineral Deposit Research: Meeting the Global Challenge, 405–7. Berlin, Heidelberg: Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_106.

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Burrows, D. R., and C. M. Lesher. "Copper-Rich Magmatic Ni-Cu-PGE Deposits." In Geology and Genesis of Major Copper Deposits and Districts of the WorldA Tribute to Richard H. Sillitoe. Society of Economic Geologists, 2012. http://dx.doi.org/10.5382/sp.16.20.

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Konnunaho, J., T. Halkoaho, E. Hanski, and T. Törmänen. "Komatiite-Hosted Ni-Cu-PGE Deposits in Finland." In Mineral Deposits of Finland, 93–131. Elsevier, 2015. http://dx.doi.org/10.1016/b978-0-12-410438-9.00004-2.

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Conference papers on the topic "Ni-Cu-PGE deposits"

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Balch, S. J. "Exploration strategies for small high‐grade Ni‐Cu‐PGE deposits." In SEG Technical Program Expanded Abstracts 2002. Society of Exploration Geophysicists, 2002. http://dx.doi.org/10.1190/1.1817268.

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Morrison, Jean M., Andrew H. Manning, and Richard B. Wanty. "METAL CONCENTRATIONS IN COVER OVERLYING DULUTH COMPLEX NI-CU-PGE DEPOSITS, NE MINNESOTA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285031.

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Vidyadharan, K. T., P. Krishnamurthy, and R. H. Sawkar. "Exploration Strategies for Ni-Cu-PGE and Chromite in the Ultramafic-Mafic and Related Rocks of Karnataka, India." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63390.

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Dora, M. L., A. Kundu, M. Shareef, S. Shome, S. Joshi, and K. Koteswar Rao. "Ni-Cu-PGE Mineralization of Heti Prospect, Western Bastar Craton, Central India: An Appraisal Based on Petrographic, SEM and EPMA Study." In Proceedings of the Workshop on Magmatic Ore Deposits. Geological Society of India, 2015. http://dx.doi.org/10.17491/cgsi/2014/63387.

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Manning, Andrew H., Richard B. Wanty, Jean M. Morrison, and Stefania Da Pelo. "CHEMICAL SIGNATURE OF GROUNDWATER IN COVER OVERLYING DULUTH COMPLEX NI-CU-PGE DEPOSITS, NE MINNESOTA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-279731.

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Benson, Erin, Edward M. Ripley, Chusi Li, and Robert Mahin. "MULTIPLE SULFUR ISOTOPE STUDY OF EAGLE EAST, MICHIGAN: UNDERSTANDING THE GENESIS OF NI-CU-PGE DEPOSITS." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-311727.

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Mansur, Eduardo, Sarah-Jane Barnes, and Charley J. Duran. "AN OVERVIEW OF CHALCOPHILE ELEMENT CONTENTS OF PYRRHOTITE, PENTLANDITE, CHALCOPYRITE AND PYRITE FROM MAGMATIC NI-CU- PGE DEPOSITS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-355847.

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Larsen, R. B., Bjørn Eske Sørensen, and Lars Tollefsrud. "FORMATION OF PGE-CU-NI DEPOSITS IN A HIGH-YIELDING LOWER CRUSTAL PLUMBING SYSTEM: THE SEILAND IGNEOUS PROVINCE, N-NORWAY." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-319209.

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Malehmir, Alireza, Christopher Juhlin, Chris Wijns, Milovan Urosevic, Petri Valasti, Emilia koivisto, Ilmo Kukkonen, Pekka Heikkinen, and Markku Paananen. "3D reflection seismic investigation for mine planning and exploration in the Kevitsa Ni‐Cu‐PGE deposit, northern Finland." In SEG Technical Program Expanded Abstracts 2011. Society of Exploration Geophysicists, 2011. http://dx.doi.org/10.1190/1.3627427.

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Haag, Beau, and Joyashish Thakurta. "CHARACTERIZATION OF COUNTRY-ROCK HOSTED SULFIDE TEXTURES WITHIN THE VICINITY OF THE EAGLE NI-CU-PGE DEPOSIT, UPPER PENINSULA, MICHIGAN." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-331833.

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Reports on the topic "Ni-Cu-PGE deposits"

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Nixon, G. T., M. J. Manor, S. Jackson-Brown, J. S. Scoates, and D. E. Ames. Magmatic Ni-Cu-PGE sulphide deposits at convergent margins. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296676.

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Ames, D. E., I. Kjarsgaard, and B. McClenaghan. Target characterization of Footwall Cu-(Ni)-PGE deposits, Sudbury. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292379.

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Dulfer, H., R. G. Skirrow, D. C. Champion, L. M. Highet, K. Czarnota, R. Coghlan, and P. R. Milligan. Potential for intrusion-hosted Ni-Cu-PGE sulfide deposits in Australia: A continental-scale analysis of mineral system prospectivity. Geoscience Australia, 2016. http://dx.doi.org/10.11636/record.2016.001.

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Giovenazzo, D., R. Sproule, J. Simmonds, and P. K. Williams. Large scale targeting for Ni-Cu-PGE sulphide deposits using a minerals systems approach: an example from West Africa. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/300709.

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Ames, D. E., and I. Kjarsgaard. Sulphide and alteration mineral chemistry of low- and high- sulphide Cu-PGE-Ni deposits in the Footwall environment, Sudbury, Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2013. http://dx.doi.org/10.4095/292707.

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Ames, D. E., and M. G. Houlé. A synthesis of the TGI-4 Canadian nickel-copper-platinum group elements-chromium ore systems project -- revised and new genetic models and exploration tools for Ni-Cu-PGE, Cr-(PGE), Fe-Ti-V-(P), and PGE-Cu deposits. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296675.

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Jefferson, C. W., L. J. Hulbert, R. H. Rainbird, G. E. M. Hall, D C Grégoire, and L. I. Grinenko. Mineral resource assessment of the Neoproterozoic Franklin Igneous Events of Arctic Canada: comparison with the Permo-Triassic Noril'sk-Talnakh Ni-Cu-PGE deposits of Russia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/193362.

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Houlé, M. G., C. M. Lesher, V. J. McNicoll, R. T. Metsaranta, A.-A. Sappin, J. Goutier, V. Bécu, H. P. Gilbert, and E M Yang. Temporal and spatial distribution of magmatic Cr-(PGE), Ni-Cu-(PGE), and Fe-Ti-(V) deposits in the Bird River--Uchi--Oxford-Stull--La Grande Rivière--Eastmain domains: a new metallogenic province within the Superior Craton. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/296677.

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Good, D. J., O. R. Eckstrand, A. Yakubchuk, and Q. Gall. World Ni-Cu-PGE-Cr deposit database. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2015. http://dx.doi.org/10.4095/297321.

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Dare, S. A. S., D. E. Ames, P. C. Lightfoot, S. J. Barnes, and G. Beaudoin. Mineral chemistry and supporting databases for TGI4 project on "Trace elements in Fe-oxides from fertile and barren igneous complexes: Investigating their use as a vectoring tool in the intrusions that host Ni-Cu-PGE deposits". Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2014. http://dx.doi.org/10.4095/293640.

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You might also be interested in the extended bibliographies on the topic 'Ni-Cu-PGE deposits' for particular source types:
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