作者: H. Porada , G. Druschel
DOI: 10.1016/J.JAFREARSCI.2010.04.006
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摘要: Abstract The Copperbelt of Zambia is the world’s largest sediment-hosted stratiform copper province, hosted in siliciclastic sediments Roan Group, which forms basal part Neoproterozoic–Paleozoic Katanga Supergroup. Much ore deposition occurred between 880 Ma and 780 Ma, on a rimmed platform consisting carbonate barrier, lagoonal basin tidal flats grading into sabkhas hinterland. Various sedimentary structures developed formation at Mindola Open Pit mine, are herein considered to be microbially induced identified as microbial shrinkage cracks, wrinkle structures, mat deformation petees, concentric microfaults, chips. occurrence these all units Mine suggests mats grew paleo-sediment surface throughout cupriferous succession. As require cohesive layers, were likely cyanobacterial type, that well aerated intertidal lower supratidal zones. Cyanobacterial typically consist layer filamentous cyanobacteria underlain by anaerobic, heterotrophic sulfate reducing bacteria (SRB). A distinct sulfide mineral zonation, major deposits Copperbelt, ranges from barren (sabkha) sediments, through chalcocite zone, bornite followed chalcopyrite pyrite subtidal zone anoxic depotcentre. This sequence minerals can modelled paragenetic mineralization resulting progressive reduction source fluid, indicating geochemical conditions formation, least, produced activity SRB.