Chromitite and platinum-group-element mineralization at middle arm brook, central advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada

We report the first find of chromitite in the mantle harzburgite of the Advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada. Chromitite occurs as centimetric veins, pods and schlieren enveloped by dunite at Middle Arm Brook. The composition of the chromian spinel is homogeneous, w...

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Autores principales: Escayola, M., Garuti, G., Zaccarini, F., Proenza, J.A., Bédard, J.H., Vanstaal, C.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00084476_v49_n6_p1523_Escayola
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spelling todo:paper_00084476_v49_n6_p1523_Escayola2023-10-03T14:06:10Z Chromitite and platinum-group-element mineralization at middle arm brook, central advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada Escayola, M. Garuti, G. Zaccarini, F. Proenza, J.A. Bédard, J.H. Vanstaal, C. Advocate complex Baie verte peninsula Canada Chromitite Middle arm brook Newfoundland Ophiolite Platinum-group elements Platinum-group minerals Advocate complex Baie verte peninsula Canada Chromitites Middle arm brook Newfoundlands Ophiolite Platinum group elements Platinum-group minerals Chromite Chromite deposits Chromium Desulfurization Igneous rocks Iridium Lithology Osmium Osmium alloys Platinum Ruthenium Ruthenium alloys Serpentine Sulfur Sulfur compounds Platinum compounds chromitite high temperature mineralization ophiolite peridotite platinum group element subduction Baie Verte Peninsula Canada Newfoundland Newfoundland and Labrador We report the first find of chromitite in the mantle harzburgite of the Advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada. Chromitite occurs as centimetric veins, pods and schlieren enveloped by dunite at Middle Arm Brook. The composition of the chromian spinel is homogeneous, with relatively high Cr# and low TiO2, and is consistent with formation of the chromitite by interaction of boninite-type basaltic melt with residual mantle in a supra-subduction arc setting. Chromitites contain up to 1028 ppb total PGE, with significant enrichment in PPGE relative to IPGE, and are characterized by a positive slope of the chondrite-normalized patterns. This is uncommon in typical ophiolitic chromitites, and distinguishes the Middle Arm Brook chromitites from those in the mantle harzburgite of other Appalachian ophiolites (Bay of Island and Thetford Mines), which usually display negative PGE patterns with low Pd/Ir values. The PGM assemblage consists of sulfides (laurite and an undefined Ir-S phase), native PGE (osmium, ruthenium), PPGE - base-metal alloys and PPGE antimonides. The textural characteristics of the IPGE sulfides suggests that they are magmatic in origin. In contrast, the PPGE minerals invariably occur associated with low-temperature alteration phases (ferrian chromite, Fe oxides, serpentine, chlorite, brucite, awaruite, heazlewoodite, and Co-rich pentlandite). The PPGE alloys are interpreted to represent the product of desulfurization of a primary sulfide precursor, which had segregated at a high temperature interstitially to the chromite. This fact is unusual for sulfide-undersaturated boninites, and indicates that sulfide saturation was reached during the late stage of chromite precipitation, possibly by assimilation of sulfur from the country-rock mantle peridotite. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00084476_v49_n6_p1523_Escayola
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Advocate complex
Baie verte peninsula
Canada
Chromitite
Middle arm brook
Newfoundland
Ophiolite
Platinum-group elements
Platinum-group minerals
Advocate complex
Baie verte peninsula
Canada
Chromitites
Middle arm brook
Newfoundlands
Ophiolite
Platinum group elements
Platinum-group minerals
Chromite
Chromite deposits
Chromium
Desulfurization
Igneous rocks
Iridium
Lithology
Osmium
Osmium alloys
Platinum
Ruthenium
Ruthenium alloys
Serpentine
Sulfur
Sulfur compounds
Platinum compounds
chromitite
high temperature
mineralization
ophiolite
peridotite
platinum group element
subduction
Baie Verte Peninsula
Canada
Newfoundland
Newfoundland and Labrador
spellingShingle Advocate complex
Baie verte peninsula
Canada
Chromitite
Middle arm brook
Newfoundland
Ophiolite
Platinum-group elements
Platinum-group minerals
Advocate complex
Baie verte peninsula
Canada
Chromitites
Middle arm brook
Newfoundlands
Ophiolite
Platinum group elements
Platinum-group minerals
Chromite
Chromite deposits
Chromium
Desulfurization
Igneous rocks
Iridium
Lithology
Osmium
Osmium alloys
Platinum
Ruthenium
Ruthenium alloys
Serpentine
Sulfur
Sulfur compounds
Platinum compounds
chromitite
high temperature
mineralization
ophiolite
peridotite
platinum group element
subduction
Baie Verte Peninsula
Canada
Newfoundland
Newfoundland and Labrador
Escayola, M.
Garuti, G.
Zaccarini, F.
Proenza, J.A.
Bédard, J.H.
Vanstaal, C.
Chromitite and platinum-group-element mineralization at middle arm brook, central advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada
topic_facet Advocate complex
Baie verte peninsula
Canada
Chromitite
Middle arm brook
Newfoundland
Ophiolite
Platinum-group elements
Platinum-group minerals
Advocate complex
Baie verte peninsula
Canada
Chromitites
Middle arm brook
Newfoundlands
Ophiolite
Platinum group elements
Platinum-group minerals
Chromite
Chromite deposits
Chromium
Desulfurization
Igneous rocks
Iridium
Lithology
Osmium
Osmium alloys
Platinum
Ruthenium
Ruthenium alloys
Serpentine
Sulfur
Sulfur compounds
Platinum compounds
chromitite
high temperature
mineralization
ophiolite
peridotite
platinum group element
subduction
Baie Verte Peninsula
Canada
Newfoundland
Newfoundland and Labrador
description We report the first find of chromitite in the mantle harzburgite of the Advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada. Chromitite occurs as centimetric veins, pods and schlieren enveloped by dunite at Middle Arm Brook. The composition of the chromian spinel is homogeneous, with relatively high Cr# and low TiO2, and is consistent with formation of the chromitite by interaction of boninite-type basaltic melt with residual mantle in a supra-subduction arc setting. Chromitites contain up to 1028 ppb total PGE, with significant enrichment in PPGE relative to IPGE, and are characterized by a positive slope of the chondrite-normalized patterns. This is uncommon in typical ophiolitic chromitites, and distinguishes the Middle Arm Brook chromitites from those in the mantle harzburgite of other Appalachian ophiolites (Bay of Island and Thetford Mines), which usually display negative PGE patterns with low Pd/Ir values. The PGM assemblage consists of sulfides (laurite and an undefined Ir-S phase), native PGE (osmium, ruthenium), PPGE - base-metal alloys and PPGE antimonides. The textural characteristics of the IPGE sulfides suggests that they are magmatic in origin. In contrast, the PPGE minerals invariably occur associated with low-temperature alteration phases (ferrian chromite, Fe oxides, serpentine, chlorite, brucite, awaruite, heazlewoodite, and Co-rich pentlandite). The PPGE alloys are interpreted to represent the product of desulfurization of a primary sulfide precursor, which had segregated at a high temperature interstitially to the chromite. This fact is unusual for sulfide-undersaturated boninites, and indicates that sulfide saturation was reached during the late stage of chromite precipitation, possibly by assimilation of sulfur from the country-rock mantle peridotite.
format JOUR
author Escayola, M.
Garuti, G.
Zaccarini, F.
Proenza, J.A.
Bédard, J.H.
Vanstaal, C.
author_facet Escayola, M.
Garuti, G.
Zaccarini, F.
Proenza, J.A.
Bédard, J.H.
Vanstaal, C.
author_sort Escayola, M.
title Chromitite and platinum-group-element mineralization at middle arm brook, central advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada
title_short Chromitite and platinum-group-element mineralization at middle arm brook, central advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada
title_full Chromitite and platinum-group-element mineralization at middle arm brook, central advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada
title_fullStr Chromitite and platinum-group-element mineralization at middle arm brook, central advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada
title_full_unstemmed Chromitite and platinum-group-element mineralization at middle arm brook, central advocate ophiolite complex, Baie Verte Peninsula, Newfoundland, Canada
title_sort chromitite and platinum-group-element mineralization at middle arm brook, central advocate ophiolite complex, baie verte peninsula, newfoundland, canada
url http://hdl.handle.net/20.500.12110/paper_00084476_v49_n6_p1523_Escayola
work_keys_str_mv AT escayolam chromititeandplatinumgroupelementmineralizationatmiddlearmbrookcentraladvocateophiolitecomplexbaievertepeninsulanewfoundlandcanada
AT garutig chromititeandplatinumgroupelementmineralizationatmiddlearmbrookcentraladvocateophiolitecomplexbaievertepeninsulanewfoundlandcanada
AT zaccarinif chromititeandplatinumgroupelementmineralizationatmiddlearmbrookcentraladvocateophiolitecomplexbaievertepeninsulanewfoundlandcanada
AT proenzaja chromititeandplatinumgroupelementmineralizationatmiddlearmbrookcentraladvocateophiolitecomplexbaievertepeninsulanewfoundlandcanada
AT bedardjh chromititeandplatinumgroupelementmineralizationatmiddlearmbrookcentraladvocateophiolitecomplexbaievertepeninsulanewfoundlandcanada
AT vanstaalc chromititeandplatinumgroupelementmineralizationatmiddlearmbrookcentraladvocateophiolitecomplexbaievertepeninsulanewfoundlandcanada
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