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1000 Titel
  • Epithermal Ag–Au mineralization at Galim-Legalgorou, Cameroon Volcanic Line: insights from alteration mineralogy and mineral chemistry of electrum and sphalerite
1000 Autor/in
  1. Ngang, Terence Cho |
  2. Suh, Cheo Emmanuel |
  3. Wagner, Thomas |
  4. Bafon, Tasin Godlove |
  5. Fusswinkel, Tobias |
  6. Vishiti, Akumbom |
1000 Verlag Springer Berlin Heidelberg
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-05-21
1000 Erschienen in
1000 Quellenangabe
  • 113(5):1285-1301
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1007/s00531-024-02427-5 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:title>Abstract</jats:title><jats:p>The Galim-Legalgorou area, located along the north-western branch of the Cameroon Volcanic Line (CVL), is known for artisanal gold mining and primary gold exploration, but the style and origin of the mineralization has not been fully described in the scientific literature. The close spatial association of the mineralization with Tertiary volcanic rocks raises the question of whether or not this is an epithermal system in a region where all previously studied gold occurrences have been classified as orogenic. In this contribution, we use ore mineral and alteration assemblage and mineral microchemistry to constrain the origin and evolution of the mineralization. Gold is alloyed mainly with Ag (max. 53.1 wt%) and show fineness values that vary 379 and 721 with an average of 455. A cumulative percentile plot of Ag concentrations in the cores of all electrum particles, and the observed step-change from Au-rich cores to more Ag-rich mantles in zoned electrum particles, suggest that the mineralization was deposited by two distinct hydrothermal fluid influxes. The observed ore mineral association-electrum, Se/Tl-acanthite, pyrite, Fe-rich sphalerite, ± galena; the measured FeS contents of sphalerite (average 23.1 mol%), and the presence of colloform banded chalcedony and hydrothermal breccia are all consistent with features of low sulfidation epithermal deposits. This study, therefore, demonstrates for the first time, the presence of significant low sulfidation epithermal Ag–Au mineralization on the CVL, an intracontinental rift region only previously known for orogenic gold mineralization.</jats:p> <jats:p><jats:bold>Graphical Abstract</jats:bold></jats:p>
1000 Sacherschließung
lokal Galim-Legalgorou
lokal Epithermal mineralization
lokal Cameroon Volcanic Line
lokal Alteration
lokal Original Paper
lokal Low sulfidation
lokal Electrum
1000 Fächerklassifikation (DDC)
1000 Liste der Beteiligten
  1. https://orcid.org/0009-0009-5358-5253|https://frl.publisso.de/adhoc/uri/U3VoLCBDaGVvIEVtbWFudWVs|https://frl.publisso.de/adhoc/uri/V2FnbmVyLCBUaG9tYXM=|https://frl.publisso.de/adhoc/uri/QmFmb24sIFRhc2luIEdvZGxvdmU=|https://frl.publisso.de/adhoc/uri/RnVzc3dpbmtlbCwgVG9iaWFz|https://frl.publisso.de/adhoc/uri/VmlzaGl0aSwgQWt1bWJvbQ==
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  1. German Academic Exchange Service |
  2. Deutsche Forschungsgemeinschaft |
  3. RWTH Aachen University |
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    1000 Förderer German Academic Exchange Service |
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    1000 Förderer Deutsche Forschungsgemeinschaft |
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    1000 Fördernummer -
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    1000 Förderer RWTH Aachen University |
    1000 Förderprogramm -
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1000 Objektart article
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1000 Erstellt am 2025-07-06T13:49:19.387+0200
1000 Erstellt von 322
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1000 Zuletzt bearbeitet 2025-07-31T15:19:25.641+0200
1000 Objekt bearb. Thu Jul 31 15:19:25 CEST 2025
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