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    <subfield code="a">10.1016/j.jafrearsci.2025.105915</subfield>
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    <subfield code="2">sideral</subfield>
    <subfield code="a">146644</subfield>
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    <subfield code="a">ART-2025-146644</subfield>
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  <datafield tag="041" ind1=" " ind2=" ">
    <subfield code="a">eng</subfield>
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  <datafield tag="100" ind1=" " ind2=" ">
    <subfield code="a">Hajjar, Zaineb</subfield>
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  <datafield tag="245" ind1=" " ind2=" ">
    <subfield code="a">An overview of the Co-Ni-Fe arsenide ore zoning in the Bou Azzer mining district (Central Anti-Atlas, Morocco)</subfield>
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    <subfield code="c">2025</subfield>
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    <subfield code="a">Co-Ni-Fe-bearing arsenide ores in the Bou Azzer district (Anti-Atlas, Morocco) occur alongside serpentinite and are mainly found as contact-type ores or serpentinite-hosted ores. There is a clear zoning pattern in the contact-type ores, evolving from Ni-Co ores and Co-Ni ores filling fault-related open spaces at the serpentinite contact to Fe-Co types within the serpentinite itself. This trend is supported by drill core geochemistry. In serpentinite-hosted orebodies, the arsenide minerals are primarily Fe-Co ores, which preserve cores of Co-Fe ores. Our key contribution is to identify the chemical evolution of the ore-forming fluid. Co and Fe enrichment facilitated the progressive transition from Ni-Co to Co-Fe ores, while subsequent Ni depletion and Fe enrichment generated the disseminated Co-Fe ores (i.e., contact-type ores). Further circulation of these ore-forming fluids through intra-serpentinite weak fault zones tends to precipitate Fe-Co ores surrounding Co-Fe ores (i.e., serpentinite-hosted ores). Critically, we show that the established west-to-east district zoning (decreasing Co, increasing Ni) is specific to contact-type ores and may be influenced by the composition of the adjacent country rock (high Ni content is related to mafic layer in the contact. Serpentinite-hosted ores in the Ait Ahmane area appear to follow this west-east zoning process.</subfield>
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    <subfield code="9">info:eu-repo/grantAgreement/ES/MCIU/RTI2018-099157-A-I00</subfield>
    <subfield code="9">info:eu-repo/grantAgreement/ES/MINECO/RYC-2015-17596</subfield>
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    <subfield code="9">info:eu-repo/semantics/closedAccess</subfield>
    <subfield code="a">All rights reserved</subfield>
    <subfield code="u">http://www.europeana.eu/rights/rr-f/</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Fanlo, Isabel</subfield>
    <subfield code="u">Universidad de Zaragoza</subfield>
    <subfield code="0">(orcid)0000-0002-0302-2737</subfield>
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  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Ilmen, Said</subfield>
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    <subfield code="a">Bendaoud, Rachida</subfield>
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    <subfield code="a">Gervilla, Fernando</subfield>
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  <datafield tag="710" ind1="2" ind2=" ">
    <subfield code="1">2000</subfield>
    <subfield code="2">120</subfield>
    <subfield code="a">Universidad de Zaragoza</subfield>
    <subfield code="b">Dpto. Ciencias de la Tierra</subfield>
    <subfield code="c">Área Cristalografía Mineralog.</subfield>
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  <datafield tag="773" ind1=" " ind2=" ">
    <subfield code="g">234 (2025), 105915 [16 pp.]</subfield>
    <subfield code="p">J. Afr. earth sci.</subfield>
    <subfield code="t">Journal of African Earth Sciences</subfield>
    <subfield code="x">1464-343X</subfield>
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    <subfield code="a">2025-12-12-14:42:51</subfield>
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