MANGANESE IN SEAWATER AND MARINE MANGANESE BALANCE

[1] ANDERSON RN, 1972, GEOL SOC AM BULL, V83, P2947, DOI 10.1130/0016-7606(1972)83[2947:PSOLHF]2.0.CO

[2] 2

[3] GEOCHEMISTRY OF THREE CORES FROM EAST PACIFIC RISE [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1971, 12 (04) : 425 - &

[4] ACCUMULATION RATES OF MANGANESE IN PELAGIC SEDIMENTS AND NODULES [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1970, 8 (02) : 143 - &

[5] DOES UPWARD DIFFUSION SUPPLY EXCESS MANGANESE IN PELAGIC SEDIMENTS [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1971, 76 (18): : 4212 - &

[6] MANGANESE NODULES - THEIR EVOLUTION [J]. SCIENCE, 1966, 151 (3708) : 325 - &

[7] DISTRIBUTION OF TRACE METALS IN CORES FROM A TRAVERSE ACROSS INDIAN OCEAN [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1969, 33 (02) : 292 - &

[8] SEAWATER-BASALT INTERACTION AT 200 DEGREESC AND 500 BARS - IMPLICATIONS FOR ORIGIN OF SEA-FLOOR HEAVY-METAL DEPOSITS AND REGULATION OF SEAWATER CHEMISTRY [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1975, 25 (03) : 385 - 397

[9] PROVENANCE AND ACCUMULATION RATES OF OPALINE SILICA, AL, TI, FE, MN, CU, NI AND CO IN PACIFIC PELAGIC SEDIMENTS [J]. CHEMICAL GEOLOGY, 1973, 11 (02) : 123 - 148

[10] PRECIPITATES FROM HYDROTHERMAL EXHALATIONS ON EAST PACIFIC RISE [J]. ECONOMIC GEOLOGY, 1966, 61 (07) : 1258 - &

[1] ANDERSON RN, 1972, GEOL SOC AM BULL, V83, P2947, DOI 10.1130/0016-7606(1972)83[2947:PSOLHF]2.0.CO

[2] 2

[3] GEOCHEMISTRY OF THREE CORES FROM EAST PACIFIC RISE [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1971, 12 (04) : 425 - &

[4] ACCUMULATION RATES OF MANGANESE IN PELAGIC SEDIMENTS AND NODULES [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1970, 8 (02) : 143 - &

[5] DOES UPWARD DIFFUSION SUPPLY EXCESS MANGANESE IN PELAGIC SEDIMENTS [J]. JOURNAL OF GEOPHYSICAL RESEARCH, 1971, 76 (18): : 4212 - &

[6] MANGANESE NODULES - THEIR EVOLUTION [J]. SCIENCE, 1966, 151 (3708) : 325 - &

[7] DISTRIBUTION OF TRACE METALS IN CORES FROM A TRAVERSE ACROSS INDIAN OCEAN [J]. GEOCHIMICA ET COSMOCHIMICA ACTA, 1969, 33 (02) : 292 - &

[8] SEAWATER-BASALT INTERACTION AT 200 DEGREESC AND 500 BARS - IMPLICATIONS FOR ORIGIN OF SEA-FLOOR HEAVY-METAL DEPOSITS AND REGULATION OF SEAWATER CHEMISTRY [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1975, 25 (03) : 385 - 397

[9] PROVENANCE AND ACCUMULATION RATES OF OPALINE SILICA, AL, TI, FE, MN, CU, NI AND CO IN PACIFIC PELAGIC SEDIMENTS [J]. CHEMICAL GEOLOGY, 1973, 11 (02) : 123 - 148

[10] PRECIPITATES FROM HYDROTHERMAL EXHALATIONS ON EAST PACIFIC RISE [J]. ECONOMIC GEOLOGY, 1966, 61 (07) : 1258 - &