973 resultados para Mines and mineral resources -- Catalonia -- Osor

Contents of liquid hydrocarbons and their group composition in bottom sediments of the Barents Sea sampled from R/V Ivan Petrov in 2005

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(Table 2) Contents and speciations of rare earth and other chemical elements in Fe-Mn micronodules, nodules, and bottom sediments at Station DM41-3915

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Heavy mineral composition of 0.100-0.050 mm size fraction of bottom sediments from the Barents Sea sampled from R/V Krilon in 2005

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Heavy mineral composition of 0.100-0.050 mm size fraction from Barents Sea sediments, Core PL-96-101 sampled from R/V Professor Logachev in 1996

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Heavy mineral composition of 0.100-0.050 mm size fraction from Barents Sea sediments, Core PL-96-109 sampled from R/V Professor Logachev in 1996

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Heavy mineral composition of 0.1-0.05 mm grain size fraction from Kara Sea sediments

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Heavy mineral composition of 0.100-0.050 mm grain size fraction of sediments from Hole VNIIO-1990-27 drilled at the Kanin Peninsula

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Eh, pH and contents of Fe, Mn, organic carbon, CaCO3, Mo, and W in bottom sediments of the Stromboli Canyon at Station PGS-1960

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(Table 2a) Light mineral composition of 0.050-0.100 mm grain size fraction from recent bottom sediments of the Mariana Trench

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(Table 4) Rare earth element contents in Fe-Mn nodules and host sediments of the Black Sea

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Grain size composition of sediments and sedimentary rocks from Hole Nagursk-1 drilled in the Franz Josef Land Archipelago

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(Table 3-2) Concentrations particulate organic carbon, carbonate carbon, total carbon and d13C-Corg values in suspended mater from the most surface layer of bottom sediments collected by Niemistoe corers in the White Sea in July 2010

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(Table 1) Chemical composition of iron-manganese and phosphate rocks from aseismic ridges of the Indian Ocean

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(Table 4) Chemical composition of lamellae of phase X (anomalous chalcopyrite) in iss exsolution structures of the Logachev-1 and Logachev-2 hydrothermal fields

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(Table 6) Chemical composition of homogenous phase Y from copper sulfide hydrothemal chimneys of the Rainbow hydrothermal field and of lamellae in exsolution structures of the Logatchev-2 hydrothermal field

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