{"refrec":{"BRefID":77142,"RR":"<b>Le Suave, R.; Pichocki-Seyfried, C.; Pautot, G.; Hoffer, M.; Morel, Y.; Voisset, M.; Monti, S.; Amossé, J.; Kosakevitch, A.</b> (1989). Geological and mineralogical study of Co-rich ferromanganese crusts from a submerged atoll in the Tuamotu Archipelago (French Polynesia). <i>Mar. Geol. 87(2-4)</i>: 227-247","BEntID":72740,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Mar. Geol. 87(2-4)</i>: 227-247","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Le Suave, R.; Pichocki-Seyfried, C.; Pautot, G.; Hoffer, M.; Morel, Y.; Voisset, M.; Monti, S.; Amossé, J.; Kosakevitch, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Le Suave, R. <i>et al.</i>","Englishabstract":"The Tuamotu Archipelago in French Polynesia is a Co-rich ferromanganese crust pronvice. The NODCO I survey (1986) provided detailed data on Co-rich crusts in this environment through the exploration of a restricted zone in the vicinity of Niau Island on the southern flnak of the archipelago. This flat zone is a fossil atoll which, under the action the action of subsidence and tectonic movements, has collapsed to a water depth of 1000 m. Outcrops of ferromanganese crusts, are located on the inner side of the coral reef which bounds the ancient lagoon. Poorly crystallized delta -MnO<sub>2</sub>) is the dominant mineralogical phase. Cobalt enrichment seems to be related to delta -MnO<sub>2</sub> particle size. 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