FN Archimer Export Format PT J TI Origin and Composition of Ferromanganese Deposits of New Caledonia Exclusive Economic Zone BT AF Staszak, Paul Collot, Julien Josso, Pierre Pelleter, Ewan Etienne, Samuel Patriat, Martin Cheron, Sandrine Boissier, Audrey Guyomard, Yaël AS 1:1,2;2:1;3:3;4:2;5:1;6:2;7:2;8:2;9:1; FF 1:PDG-REM-GM-LAD;2:;3:;4:PDG-REM-GEOOCEAN-CYBER;5:;6:PDG-REM-GEOOCEAN-ALMA;7:PDG-REM-GEOOCEAN-CYBER;8:PDG-REM-GEOOCEAN-CYBER;9:; C1 Geological Survey of New Caledonia, Direction de l’Industrie, des Mines et de l’Énergie de Nouvelle-Calédonie, BP M2, Nouméa 98845, New Caledonia Institut Français de Recherche pour l’Exploitation de la Mer (IFREMER), Unité Géosciences Marines, 29280 Plouzané, France British Geological Survey, Environmental Science Centre, Nottingham NG12 5GG, UK C2 DIMENC SERV GEOL NOUVELLE CALEDONIE, FRANCE IFREMER, FRANCE BRITISH GEOL SURVEY, UK SI NOUMEA BREST SE PDG-REM-GM-LAD PDG-REM-GEOOCEAN-CYBER PDG-REM-GEOOCEAN-ALMA UM GEO-OCEAN IN WOS Ifremer UMR DOAJ copubli-france copubli-europe IF 2.5 TC 4 UR https://archimer.ifremer.fr/doc/00751/86344/91665.pdf https://archimer.ifremer.fr/doc/00751/86344/91666.zip LA English DT Article CR BATHUS 3 EBISCO ECO GEORSTOM III EVA 76/1 EVA 76/2 GEORSTOM II GEORSTOM III EST GEORSTOM III NORD GEORSTOM III SUD IPOD KANADEEP 1 KANADEEP 2 VESPA BO Alis Le Noroit Coriolis L'Atalante DE ;ferromanganese crusts;New Caledonia;hydrogenetic;hydrothermal and diagenetic deposits AB Located in the South-West Pacific, at the northern extremity of the mostly submerged Zealandia continent, the New Caledonian Exclusive Economic Zone (EEZ) covers 1,470,000 km² and includes basins, ridges and seamounts where abundant ferromanganese crusts have been observed. Several investigations have been conducted since the 1970s on the nature and composition of ferromanganese crusts from New Caledonia’s seamounts and ridges, but none have covered the entire EEZ. We present data from 104 ferromanganese crusts collected in New Caledonia’s EEZ during twelve oceanographic cruises between 1974 and 2019. Samples were analysed for mineralogy, geochemical compositions, growth rates, and through a statistical approach using correlation coefficients and factor analysis. Crust thicknesses range from 1 mm to 115 mm, with growth rates between 0.45 mm/Ma and 102 mm/Ma. Based on textures, structures, discrimination plots, and growth rates, we distinguish a group of hydrogenetic crusts containing the highest mean contents of Co (0.42 wt%), Ni (0.31 wt%), and high contents of Mo, V, W, Pb, Zn, Nb, from a group of hydrothermal and/or diagenetic deposits showing high mean contents of Mn (38.17 wt%), Ba (0.56 wt%) and low contents of other trace metals. Several samples from this later group have exceptionally high content of Ni (0.7 wt%). The data shows that crusts from the southern part of the EEZ, notably seamounts of the Loyalty Ridge and the Lord Howe Rise, present high mineral potential for prospectivity owing to high contents of valuable metals, and constitute a great target for further investigation. PY 2022 PD FEB SO Minerals SN 2075-163X PU MDPI AG VL 12 IS 2 UT 000762562000001 DI 10.3390/min12020255 ID 86344 ER EF