Search Results - "Thompson, John F. H."

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    Formation of giant iron oxide-copper-gold deposits by superimposed episodic hydrothermal pulses by del Real, Irene, Reich, Martin, Simon, Adam C., Deditius, Artur, Barra, Fernando, Rodríguez-Mustafa, María A., Thompson, John F. H., Roberts, Malcolm P.

    Published in Scientific reports (25-07-2023)
    “…Iron oxide-copper-gold (IOCG) deposits are a globally important source of copper, gold and critical commodities. Despite their relevance, IOCG deposits remain…”
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  2. 2

    Future availability of non-renewable metal resources and the influence of environmental, social, and governance conflicts on metal production by Jowitt, Simon M., Mudd, Gavin M., Thompson, John F. H.

    Published in Communications earth & environment (01-09-2020)
    “…Metal mining provides the elements required for the provision of energy, communication, transport and more. The increasing uptake of green technology, such as…”
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    RETRACTED ARTICLE: Formation of giant iron oxide-copper-gold deposits by superimposed, episodic hydrothermal pulses by Del Real, Irene, Reich, Martin, Simon, Adam C., Deditius, Artur, Barra, Fernando, Rodríguez-Mustafa, María A., Thompson, John F. H., Roberts, Malcolm P.

    Published in Communications earth & environment (01-12-2021)
    “…Iron oxide-copper-gold deposits are a globally important source of copper, gold and critical commodities. However, they possess a range of characteristics…”
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    Journal Article
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    Spatially and temporally associated porphyry deposits with distinct Cu/Au/Mo ratios, Woodjam District, central British Columbia by del Real, Irene, Bouzari, Farhad, Rainbow, Amelia, Bissig, Thomas, Blackwell, Jacqueline, Sherlock, Ross, Thompson, John F. H, Hart, Craig J. R

    “…The Woodjam district is a cluster of porphyry Cu-Au deposits of Early Jurassic age (∼196 Ma) and is located in the Quesnel terrane in central British Columbia…”
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    High sulfidation deposits in the volcanogenic massive sulfide environment by Sillitoe, Richard H, Hannington, Mark D, Thompson, John F. H

    “…Volcanogenic massive sulphide mineralization is formed on or immediately beneath the sea-floor by the discharge of hydrothermal fluids. This has implications…”
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    Evidence for transpression during formation of the Candelaria Punta del Cobre IOCG -district and regional implications by del Real, Irene, Allmendinger, Richard W., Thompson, John F.H., Creixell, Christian

    Published in Journal of South American earth sciences (01-06-2023)
    “…The youngest and best exposed Iron Oxide Cu–Au (IOCG) deposits currently recognized are found in the coastal belt of the Andes. Their formation has been…”
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  12. 12

    Metallogeny of an Early to Middle Jurassic arc, Iskut River area, northwestern British Columbia by Macdonald, A. James, Lewis, Peter D, Thompson, John F. H, Nadaraju, Genga, Bartsch, Roland, Bridge, David J, Rhys, David A, Roth, Tina, Kaip, Andrew, Godwin, Colin I, Sinclair, Alastair J

    “…The Iskut River area of northwestern British Columbia is a relatively small (approx 100 x 60 km) but metallogenetically significant portion of the Canadian…”
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    Intrusion-Related Vein Gold Deposits: Types, Tectono-Magmatic Settings and Difficulties of Distinction from Orogenic Gold Deposits by SILLITOE, Richard H., THOMPSON, John F. H.

    Published in Resource geology (01-12-1998)
    “…: A spectrum of intrusion‐related vein gold deposits is recognized. Representative examples are described of the following geochemical associations: Au‐Fe…”
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    The Dublin Gulch intrusion-hosted gold deposit, Tombstone plutonic suite, Yukon Territory, Canada by Maloof, Terri, Baker, Timothy, Thompson, John

    Published in Mineralium deposita (01-09-2001)
    “…The Dublin Gulch intrusion is a member of the Tombstone plutonic suite, a linear belt of middle Cretaceous intrusions that extend across the Yukon Territory…”
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    The geology of the Vakkerlien nickel prospect, Kvikne, Norway by THOMPSON, J. F. H, NIXON, F, SIVERTSEN, R

    “…The Vakkerlien nickel prospect is a small sulfide mineralized zone centrally located within a metagabbro body. The body, and a second barren metagabbro, are…”
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