Bender, Michael L. (1983): Pore water chemistry of the Mounds Hydrothermal Field, Galapagos spreading center; results from Glomar Challenger piston coring

Leg/Site/Hole:
DSDP 70
DSDP 70 506
DSDP 70 507
DSDP 70 508
DSDP 70 509
Identifier:
1983-024678
georefid

10.1029/JB088iB02p01049
doi

Creator:
Bender, Michael L.
Univ. R.I., Grad. Sch. Oceanogr., Kingston, RI, United States
author

Identification:
Pore water chemistry of the Mounds Hydrothermal Field, Galapagos spreading center; results from Glomar Challenger piston coring
1983
Journal of Geophysical Research
American Geophysical Union, Washington, DC, United States
88
B2
1049-1056
MnO (sub 2) -encrusted nontronite mounds. Analyses are presented for Ca, Mg, Si, NH (sub 3) , Mn, and Fe. Results confirm conclusions that hydrothermal solutions enriched in Ca by 1-2 mM and depleted in Mg by approximately 2 mM are upwelling through the mounds and the surrounding pelagic sediments. Si, NH (sub 3) , and Mn (super 2+) concentrations generally increase upcore. The formation of nontronite (Fe(III) (sub 4) Si (sub 8) O (sub 20) (OH) (sub 4) ) involves oxidation of dissolved Fe (super 2+) . Fe (super 2+) oxidation by MnO (sub 2) and replacement of MnO (sub 2) by nontronite at the base of the MnO (sub 2) crust, followed by upward migration of Mn (super 2+) and precipitation of MnO (sub 2) at the sediment water surface.--Modified journal abstract.
Coverage:Geographic coordinates:
North:0.3700
West:-86.1000East: -86.0500
South:0.3200

Geochemistry of rocks, soils, and sediments; areal studies; clay mineralogy; clay minerals; cores; Deep Sea Drilling Project; DSDP Site 506; DSDP Site 507; DSDP Site 508; DSDP Site 509; East Pacific; Galapagos Rift; geochemistry; hydrothermal conditions; IPOD; Leg 70; marine sediments; minerals; mounds; Mounds Hydrothermal Field; nontronite; oxidation; Pacific Ocean; pore water; sediments; sheet silicates; silicates; South American Pacific; South Pacific; Southeast Pacific;

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