Transition metal mobility and recoverability from weathered serpentinite and serpentinite skarn tailings from Lord Brassey Mine, Australia and Record Ridge, British Columbia, Canada

dc.contributor.authorHonda-McNeil, Men_AU
dc.contributor.authorWilson, SAen_AU
dc.contributor.authorLocock, Aen_AU
dc.contributor.authorMililli, Ben_AU
dc.contributor.authorZeyen, Nen_AU
dc.contributor.authorWang, Ben_AU
dc.contributor.authorTurvey, Cen_AU
dc.contributor.authorVessey, CJen_AU
dc.contributor.authorPatel, ASen_AU
dc.contributor.authorHamilton, JLen_AU
dc.contributor.authorSoutham, Gen_AU
dc.contributor.authorPoitras, Jen_AU
dc.contributor.authorJones, TRen_AU
dc.contributor.authorJowitt, Sen_AU
dc.contributor.authorLowock, Aen_AU
dc.date.accessioned2023-12-13T02:34:40Zen_AU
dc.date.available2023-12-13T02:34:40Zen_AU
dc.date.issued2022-07-14en_AU
dc.date.statistics2023-03-30en_AU
dc.description.abstractAs mineral resources become scarcer, companies are lowering their ore cut-off grades and resorting to exploring deeper underground and in more isolated areas. Incorporating tailings storage facilities and tailings reprocessing as part of the ore processing circuit can potentially extend the lives of mines and save on future exploration costs. Ultramafic and mafic mine tailings host resources including first and second row transition metals, such as nickel (Ni), cobalt (Co), and platinum group elements (PGE), whose high value and recovery could serve as a motivator for existing mines to reprocess their tailings. Many of these target metals are initially hosted by olivine, are repartitioned during serpentinization to form sulfides, oxides and alloys, and then are remobilized during weathering to form authigenic carbonates, sulfates and oxyhydroxides. Reprocessing tailings may further provide environmental benefits, including a reduction in waste output and the ability to offset greenhouse gas emissions by enhanced silicate-weathering and carbonation reactions. Here we use powder X-ray diffraction, scanning electron microscopy, electron probe micro-analysis and synchrotron X-ray fluorescence mapping to demonstrate how first and second row transition metals are mobilized to their final sinks. Samples of serpentinite, skarn and weathered tailings from the historical Lord Brassey nickel mine in Tasmania, Australia and weathered outcrops of serpentinite ore from the proposed magnesium mine in Record Ridge, BC, Canada are analyzed and compared. Preliminary results from these climatically similar localities indicate clear transition metal dissemination patterns across alteration zones and distinct partitioning behavior (ex. homogenous distribution of Ni within sulfides) in weathering products. By developing an understanding of the sinks for metals across the mining lifecycle, we aim to cultivate an economically.en_AU
dc.identifier.citationHonda-McNeil, M., Wilson, S., Mililli, B., Zeyen, N., Wang, B., Turvey, C., Vessey, C., Patel, A., Locock A., Hamilton, J., Paterson, D. M., Southam, G., Poitras, J., Jones, T., & Jowitt, S. (2021). Transition metal mobility and recoverability from weathered serpentinite and serpentinite skarn tailings from Lord Brassey Mine, Australia and Record Ridge, British Columbia, Canada. Poster presented to 2021 Goldschmidt Conference, 4-9 July 2021, Honolulu, Hawaii, USA and Online. Retrieved from: https://goldschmidtabstracts.info/abstracts/abstractView?doi=10.7185/gold2021.4827en_AU
dc.identifier.conferenceenddate2021-07-09en_AU
dc.identifier.conferencename2021 Goldschmidt Conferenceen_AU
dc.identifier.conferenceplaceHonolulu, Hawaii, USA and Onlineen_AU
dc.identifier.conferencestartdate2021-07-04en_AU
dc.identifier.urihttps://goldschmidtabstracts.info/abstracts/abstractView?doi=10.7185/gold2021.4827en_AU
dc.identifier.urihttps://apo.ansto.gov.au/handle/10238/15286en_AU
dc.language.isoenen_AU
dc.publisherGoldschmidten_AU
dc.subjectTransition elementsen_AU
dc.subjectWeatheringen_AU
dc.subjectSerpentinitesen_AU
dc.subjectTailingsen_AU
dc.subjectMinesen_AU
dc.subjectAustraliaen_AU
dc.subjectCanadaen_AU
dc.subjectX-ray diffractionen_AU
dc.titleTransition metal mobility and recoverability from weathered serpentinite and serpentinite skarn tailings from Lord Brassey Mine, Australia and Record Ridge, British Columbia, Canadaen_AU
dc.typeConference Posteren_AU
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