Accretion rate of extraterrestrial particles determined from osmium isotope systematics of pacific pelagic clay and manganese nodules
Conference
·
· Geochimica et Cosmochimica Acta; (USA)
OSTI ID:5557526
- Yale Univ., New Haven, CT (USA)
Pelagic clay and Mn nodules from DOMES sites in the North Pacific and a varved glacial lake deposit from Connecticut were analyzed for Os concentration and isotopic composition by isotope-dilution secondary ion mass spectrometry after treatment by NiS fusion of oxalic acid leaching. Bulk pelagic clay from DOMES site C has {sup 187}Os/{sup 186}Os = 6.5 and Os = 0.14 ng/g. Oxalic acid leaches of this same sediment and of Mn nodules for DOMES sites A and C have more radiogenic {sup 187}Os/{sup 186}Os ratios which average 8.3. Bulk glacial Lake Hitchcock sediment has {sup 187}Os/{sup 186}Os = 12.5 and Os = 0.06 ng/g. The total Os flux to North Pacific pelagic clay is 7 to 10 ng Os/cm{sup 2}/10{sup 6} y. Lake Hitchcock sediment provides an integrated value for the local crustal {sup 187}Os/{sup 186}Os ratio. The oxalic acid leaches are assumed to attack hydrogenous phases selectively. A simple model in which the only sources of Os to the ocean are continental crust with the isotopic composition of Lake Hitchcock and extraterrestrial particles with {sup 187}Os/{sup 186}Os = 1.1 results in a cosmic flux of osmium to the sediment of 4.9 ng Os/cm{sup 2}/10{sub 6} y of which 20% is hydrogenous. A model in which the sources of Os to the ocean are continental crust with an {sup 187}Os/{sup 186}Os ratio of 30, oceanic mantle or crust with {sup 187}Os/{sup 186}Os = 1.04 and extraterrestrial particles with {sup 187}Os/{sup 186}Os = 1.1 results in a cosmic flux of Os to the sediment of 5.7 ng Os/cm{sup 2}/10{sup 6} y of which none is hydrogenous. These extraterrestrial Os fluxes correspond to maximum C-1 chondrite accretion rates of between 4.9 {times} 10{sub 4} and 5.6 {times}10{sub 4} tonnes/y.
- OSTI ID:
- 5557526
- Report Number(s):
- CONF-8703325--
- Conference Information:
- Journal Name: Geochimica et Cosmochimica Acta; (USA) Journal Volume: 52:6
- Country of Publication:
- United States
- Language:
- English
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CONTRIBUTION TO THE DATING OF IRON METEORITES BY THE RHENIUM-OSMIUM METHOD
Journal Article
·
Sat Nov 30 23:00:00 EST 1991
· Geochimica et Cosmochimica Acta; (United States)
·
OSTI ID:7049727
Osmium-187/osmium-186 in manganese nodules and the Cretaceous-Tertiary boundary
Journal Article
·
Thu Nov 10 23:00:00 EST 1983
· Science (Washington, D.C.); (United States)
·
OSTI ID:5314102
CONTRIBUTION TO THE DATING OF IRON METEORITES BY THE RHENIUM-OSMIUM METHOD
Journal Article
·
Sun Oct 01 00:00:00 EDT 1961
· Z. Naturforsch
·
OSTI ID:4809618
Related Subjects
58 GEOSCIENCES
580400* -- Geochemistry-- (-1989)
580500 -- Oceanography-- (1980-1989)
CHEMICAL ANALYSIS
CHEMISTRY
CHONDRITES
CLAYS
CONTINENTAL CRUST
DISSOLUTION
EARTH CRUST
GEOCHEMISTRY
GEOLOGIC DEPOSITS
GEOLOGIC MODELS
ISOTOPE RATIO
ISOTOPES
LEACHING
MANGANESE ORES
METEORITES
OCEANIC CRUST
ORES
ORIGIN
OSMIUM ISOTOPES
PACIFIC OCEAN
PRECIPITATION
SEAS
SEDIMENTS
SEPARATION PROCESSES
STONE METEORITES
SURFACE WATERS
580400* -- Geochemistry-- (-1989)
580500 -- Oceanography-- (1980-1989)
CHEMICAL ANALYSIS
CHEMISTRY
CHONDRITES
CLAYS
CONTINENTAL CRUST
DISSOLUTION
EARTH CRUST
GEOCHEMISTRY
GEOLOGIC DEPOSITS
GEOLOGIC MODELS
ISOTOPE RATIO
ISOTOPES
LEACHING
MANGANESE ORES
METEORITES
OCEANIC CRUST
ORES
ORIGIN
OSMIUM ISOTOPES
PACIFIC OCEAN
PRECIPITATION
SEAS
SEDIMENTS
SEPARATION PROCESSES
STONE METEORITES
SURFACE WATERS