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Dissertations / Theses on the topic 'Cu-PGE'

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Published: 4 June 2021

Last updated: 10 February 2022

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1

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 an

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2

Nelles, Edward William. "Genesis of Cu-PGE-rich footwall-type mineralization in the Morrison deposit, Sudbury." Thesis, Laurentian University of Sudbury, 2014. https://zone.biblio.laurentian.ca/dspace/handle/10219/2205.

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The Morrison deposit, located at the Levack mine in the City of Greater Sudbury, is a footwall-type Cu-Ni-platinum-group-element (PGE) deposit hosted within a zone of Sudbury Breccia in the Archean Levack Gneiss Complex beneath the North Range of the Sudbury Igneous Complex. It consists of sharp-walled, sulfide-rich veins that are enriched in Cu-Pt-Pd-Au relative to contact-type mineralization and can be subdivided based on vein geochemistry, mineralogy, texture, and morphology into a pyrrhotite-rich upper domain, a chalcopyrite-rich lower domain, and a pyrrhotite equal to chalcopyrite middle

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3

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 sulp

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4

Mukwakwami, Joshua. "STRUCTURAL CONTROLS OF Ni-Cu-PGE ORES AND MOBILIZATION OF METALS AT THE GARSON MINE, SUDBURY." Thesis, Laurentian University of Sudbury, 2014. https://zone.biblio.laurentian.ca/dspace/handle/10219/2129.

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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 an

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5

Hagerfors, Erika. "Formation of Sulphides in the Canadian High Arctic Large Igneous Province; Testing the Influence of Sedimentary Rocks." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-357415.

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Large Igneous Provinces (LIPs) form during short-lived pulses of extensive magmatic activity. LIPs are known for their ability to affect global climate as well as for their Ni-Cu-PGE ore potential. A key factor that controls the intensity of the climate impact of a LIP and its ore potential is the assimilation of volatile-rich sedimentary host rocks. Magmas of the High Arctic Large Igneous Province (HALIP), exposed in the Arctic, intruded volatile-rich black shales, carbonates and evaporites in the Canadian Arctic Islands, offering a great opportunity for studying magma-sediment interaction. T

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6

Augustin, Cláudia Tharis. "Evolução magmática e metamórfica da intrusão máfica ultramáfica mineralizada a Ni-Cu-PGE de Mangabal, Brasil Central." reponame:Repositório Institucional da UnB, 2018. http://repositorio.unb.br/handle/10482/32460.

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Dissertação (mestrado)—Universidade de Brasília, Instituto de Geociências, Programa de Pós-Graduação em Geologia, 2018.<br>Submitted by Fabiana Santos (fabianacamargo@bce.unb.br) on 2018-08-21T18:49:57Z No. of bitstreams: 1 2018_CláudiaTharisAugustin.pdf: 5210708 bytes, checksum: 99f53f29a2d8ff706c6e29a34801ff12 (MD5)<br>Approved for entry into archive by Raquel Viana (raquelviana@bce.unb.br) on 2018-08-21T19:18:25Z (GMT) No. of bitstreams: 1 2018_CláudiaTharisAugustin.pdf: 5210708 bytes, checksum: 99f53f29a2d8ff706c6e29a34801ff12 (MD5)<br>Made available in DSpace on 2018-08-21T19:18:25Z (GMT)

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7

Fletcher, Timothy Andrew. "The geology, mineralisation (Ni-Cu-PGE) and isotope systematics of Caledonian mafic intrusions near Huntly, NE Scotland." Thesis, University of Aberdeen, 1989. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=88127.

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The Caledonian mafic and ultramafic intrusions of the Grampian region of N.E. Scotland are a suite of synorogenic tholeiitic plutons of mid-Ordovician Age. They include layered cumulates, granular gabbronorites, quartz biotite norites and xenolithic contact facies lithologies. They postdate two regional deformation events in the enclosing Late Precambrian Dalradian metasediments, but are themselves locally deformed by a major regional ductile shear zone system. A detailed study of the Huntly-Knock area was undertaken combining geological mapping, petrological, geochemical and stable isotope te

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8

Song, Xieyan, and 宋謝炎. "Geochemistry of permian flood basalts and related ni-cu-(pge) sulfide-bearing sills in Yangliuping, Sichuan province, China." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2004. http://hub.hku.hk/bib/B3124595X.

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9

Silva, Jonas Mota e. "O depósito sulfetado Ni-Cu-(pge) de Limoeiro : metalogênese, magmatismo máfico e metamorfismo no leste da Província Borborema." reponame:Repositório Institucional da UnB, 2014. http://repositorio.unb.br/handle/10482/18079.

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Tese (doutorado)—Universidade de Brasília, Instituto de Geociências, Programa de Pós-Graduação em Geologia, 2014.<br>Submitted by Ana Cristina Barbosa da Silva (annabds@hotmail.com) on 2015-04-30T19:31:10Z No. of bitstreams: 1 2014_JonasMotaeSilva.pdf: 23053512 bytes, checksum: 47ee6942746173aecae50290d8979fb8 (MD5)<br>Approved for entry into archive by Ruthléa Nascimento(ruthleanascimento@bce.unb.br) on 2015-05-04T14:05:23Z (GMT) No. of bitstreams: 1 2014_JonasMotaeSilva.pdf: 23053512 bytes, checksum: 47ee6942746173aecae50290d8979fb8 (MD5)<br>Made available in DSpace on 2015-05-04T14:05:23Z (

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10

Viljoen, Willemien. "Phase relations in the system Cu-Fe-Ni-S and their application to the slow cooling of PGE matte." Pretoria : [s.n.], 2005. http://upetd.up.ac.za/thesis/available/etd-10132005-100921/.

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11

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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12

Rickard, Jason H. "Petrological and mineralogical study of Cu-Ni-PGE-bearing ores within the 100 orebody, Copper Cliff North mine, Sudbury, Ontario." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0012/MQ52404.pdf.

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13

Rickard, Jason H. Carleton University Dissertation Earth Sciences. "Petrological and mineralogical study of Cu-Ni-PGE-bearing ores within the 100 orebody, Copper Cliff North mine, Sudbury, Ontario." Ottawa, 2000.

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14

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 impor

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15

Jackson-Brown, Sarah. "Origin of Cu-PGE-rich sulphide mineralization in the DJ/DB zone of the Turnagain Alaskan-type intrusion, British Columbia." Thesis, University of British Columbia, 2017. http://hdl.handle.net/2429/62875.

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The Early Jurassic (>188-185 Ma) Turnagain ultramafic-mafic body, a composite Alaskan-type intrusion in the Northern Cordillera of northern British Columbia, hosts a significant nickel-cobalt resource (Horsetrail zone, 1842 Mt @ 0.21 wt. % Ni and 0.013 wt. % Co), and minor copper-platinum group element (Cu-PGE) mineralization. The 24 km² Turnagain intrusion comprises four temporally, spatially, and chemically distinct ultramafic-mafic phases that include dunite, wehrlite, clinopyroxenite, hornblendite and diorite. The 1.5 x 2 km DJ/DB zone, an area of Cu-PGE enrichment that was discovered thro

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16

Hughes, Hannah. "Temporal, lithospheric and magmatic process controls on Ni, Cu and platinum-group element (PGE) mineralisation : a case study from Scotland." Thesis, Cardiff University, 2015. http://orca.cf.ac.uk/71624/.

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A temporal and spatial relationship between plume magmatism, cratonic lithosphere and the occurrences of orthomagmatic Ni-Cu and platinum-group element (PGE) sulphide mineralisation has been documented in the literature. However the underlying causes for this correlation have yet to be resolved – is there an inherent feature of the cratonic lithosphere and its mantle ‘keel’ that controls mineralisation? Or is this correlation purely a preservational bias in the geological record? Scotland has experienced multiple tectono-magmatic events and provides an ideal testing ground, or ‘framework’, in

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17

Everest, John Owen. "The relationship of Cu-Ni-PGE veins in the Levack Gneiss Complex to contact magmatic ore at the McCreedy West Mine, Sudbury." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape8/PQDD_0016/MQ48590.pdf.

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18

Everest, John Owen Carleton University Dissertation Earth Sciences. "The Relationship of Cu-Ni-PGE veins in the Levack Gneiss complex to contact magmatic ore at the McCreedy West Mine, Sudbury." Ottawa, 1999.

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19

Fruchting, Allan. "Estratégias para utilização de dados geofísicos na exploração de mineralizações do tipo Ni-Cu-PGE : a descoberta do depósito de limoeiro, PE." reponame:Repositório Institucional da UnB, 2017. http://repositorio.unb.br/handle/10482/31000.

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Dissertação (mestrado)—Universidade de Brasília, Instituto de Geociências, Pós-Graduação em Geologia, 2017.<br>Submitted by Priscilla Sousa (priscillasousa@bce.unb.br) on 2017-11-07T13:40:28Z No. of bitstreams: 1 2017_AllanFrüchting.pdf: 3810773 bytes, checksum: 3203c84b2e476ab2127cea32ce9a5da2 (MD5)<br>Approved for entry into archive by Raquel Viana (raquelviana@bce.unb.br) on 2018-01-05T21:32:04Z (GMT) No. of bitstreams: 1 2017_AllanFrüchting.pdf: 3810773 bytes, checksum: 3203c84b2e476ab2127cea32ce9a5da2 (MD5)<br>Made available in DSpace on 2018-01-05T21:32:04Z (GMT). No. of bitstreams: 1 20

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20

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

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21

Farrow, Catharine Elizabeth Goddard Carleton University Dissertation Earth Sciences. "Geology, alteration, and the role of fluids in Cu-Ni-PGE mineralization of the footwall rocks to the Sudbury igneous complex, Levack and Morgan townships, Sudbury district, Ontario." Ottawa, 1994.

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22

Theron, Luhann Marlon. "Phase relations and Pt solubility in sulphide melt in the FE-NI-CU-S system at 1 ATM : implications for evulution of sulphide magma in the Merensky reef, Bushveld Complex, South Africa." Thesis, Stellenbosch : Stellenbosch University, 2013. http://hdl.handle.net/10019.1/80358.

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Thesis (MSc)--Stellenbosch University, 2013.<br>ENGLISH ABSTRACT: It is widely accepted that sulphide is the carrier and concentrator of PGEs during magmatic mineralization episodes in the Merensky Reef (MR). PGE concentration peaks and sulphide volume percent peaks are very closely correlated. Koegelenberg, (2011), showed in an experimental investigation that sulphide movement through a cumulate silicate and cumulate oxide pile behave in such a way that sulphide melt gets trapped in chromitite layers. When looking at the compositional distribution of sulphide within the MR it is noted that no

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23

Ruthart, Ryan. "Characterization of High-PGE Low-Sulphur Mineralization at the Marathon PGE-Cu Deposit, Ontario." Thesis, 2013. http://hdl.handle.net/10012/7382.

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The Marathon PGM-Cu deposit is hosted by the Coldwell alkaline complex, which consists predominantly of gabbro and syenite and was emplaced at 1108 Ma as part of the Mid-Continent Rift System. Mineralization at the Marathon PGM-Cu deposit is hosted by the Two Duck Lake Gabbro (TDLG), a fresh olivine-bearing gabbro. The Marathon deposit contains several zones of mineralization including the Basal Zone, the Main Zone and the W-Horizon. The W-Horizon is a high-grade PGE zone characterized by low S, low Cu/Pd and high Cu/Ni. The sulphide mineral assemblage is predominantly chalcopyrite and bornite

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24

Mealin, Caroline. "Geology, geochemistry and Cr-Ni-Cu-PGE mineralization of the Bird River sill: Evidence for a multiple intrusion model." Thesis, 2008. http://hdl.handle.net/10012/3651.

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The Bird River sill (BRS) is composed of layered mafic-ultramafic intrusive bodies which intruded the Bird River greenstone belt in southeastern Manitoba. Layered intrusions, such as those that collectively make-up the BRS, are important hosts to base and precious metal deposits. This study was initiated to examine and develop an emplacement model for the western half of the BRS and to establish the controls on Cr-Ni-Cu-PGE mineralization. The BRS intrusions were emplaced through multiple-magmatic injections into different stratigraphic levels in the Lamprey Falls Formation. It is interp

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25

White, Christopher. "Low-sulfide PGE-Cu-Ni Mineralization from Five Prospects within the Footwall of the Sudbury Igneous Complex, Ontario, Canada." Thesis, 2012. http://hdl.handle.net/1807/32849.

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North Range low-sulfide mineralization is dominantly hosted by Sudbury breccia, with amphibole-plagioclase equilibrium metamorphic temperatures of 440 to 533 ± 75oC, produced by the SICs thermal aureole. Mineralization led to increases in the bulk halogen content of the host Sudbury breccia and the formation of Ni-enriched ferromagnesian silicates. South Range low-sulfide mineralization is typically hosted by metabasalts of the Huronian Supergroup. Garnet-biotite-plagioclase-quartz geothermobarometry produced equilibrium metamorphic conditions of 513 to 645 ± 50oC and 2.0 to 7.7 ± 1.0 kbar, pr

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26

Viljoen, Willemien. "Phase relations in the system Cu-Fe-Ni-S and their application to the slow cooling of PGE matte." Thesis, 2002. http://hdl.handle.net/2263/28674.

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27

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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