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Seyfried, W.E, Bischoff, J.L (1981) Experimental seawater-basalt interaction at 300°C, 500 bars, chemical exchange, secondary mineral formation and implications for the transport of heavy metals. Geochimica et Cosmochimica Acta, 45 (2) 135-147 doi:10.1016/0016-7037(81)90157-5

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Reference TypeJournal (article/letter/editorial)
TitleExperimental seawater-basalt interaction at 300°C, 500 bars, chemical exchange, secondary mineral formation and implications for the transport of heavy metals
JournalGeochimica et Cosmochimica Acta
AuthorsSeyfried, W.EAuthor
Bischoff, J.LAuthor
Year1981 (February)Volume45
Issue2
PublisherElsevier BV
DOIdoi:10.1016/0016-7037(81)90157-5Search in ResearchGate
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Mindat Ref. ID339871Long-form Identifiermindat:1:5:339871:9
GUID0
Full ReferenceSeyfried, W.E, Bischoff, J.L (1981) Experimental seawater-basalt interaction at 300°C, 500 bars, chemical exchange, secondary mineral formation and implications for the transport of heavy metals. Geochimica et Cosmochimica Acta, 45 (2) 135-147 doi:10.1016/0016-7037(81)90157-5
Plain TextSeyfried, W.E, Bischoff, J.L (1981) Experimental seawater-basalt interaction at 300°C, 500 bars, chemical exchange, secondary mineral formation and implications for the transport of heavy metals. Geochimica et Cosmochimica Acta, 45 (2) 135-147 doi:10.1016/0016-7037(81)90157-5
In(1981, February) Geochimica et Cosmochimica Acta Vol. 45 (2) Elsevier BV

See Also

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Seyfried, W.E., Dibble, W.E. (1980) Seawater-peridotite interaction at 300°C and 500 bars: implications for the origin of oceanic serpentinites. Geochimica et Cosmochimica Acta, 44 (2) 309-321 doi:10.1016/0016-7037(80)90139-8
Seyfried, W.E., Bischoff, J.L. (1979) Low temperature basalt alteration by sea water: an experimental study at 70°C and 150°C. Geochimica et Cosmochimica Acta, 43 (12) 1937-1947 doi:10.1016/0016-7037(79)90006-1
Thornton, Edward C., Seyfried, W.E. (1987) Reactivity of organic-rich sediment in seawater at 350°c, 500 bars: experimental and theoretical constraints and implications for the guaymas basin hydrothermal system. Geochimica et Cosmochimica Acta, 51 (7) 1997-2010 doi:10.1016/0016-7037(87)90188-8
Seyfried, W.E., Chen, Xian, Chan, Lui-Heung (1998) Trace Element Mobility and Lithium Isotope Exchange During Hydrothermal Alteration of Seafloor Weathered Basalt: An Experimental Study at 350°C, 500 Bars. Geochimica et Cosmochimica Acta, 62 (6) 949-960 doi:10.1016/s0016-7037(98)00045-3
Shanks, W.C, Bischoff, James L, Rosenbauer, Robert J (1981) Seawater sulfate reduction and sulfur isotope fractionation in basaltic systems: Interaction of seawater with fayalite and magnetite at 200–350°C. Geochimica et Cosmochimica Acta, 45 (11) 1977-1995 doi:10.1016/0016-7037(81)90054-5
Seyfried, W.E, Janecky, D.R (1985) Heavy metal and sulfur transport during subcritical and supercritical hydrothermal alteration of basalt: Influence of fluid pressure and basalt composition and crystallinity. Geochimica et Cosmochimica Acta, 49 (12) 2545-2560 doi:10.1016/0016-7037(85)90123-1
Seyfried, W.E., Ding, K. (1995) The hydrothermal chemistry of fluoride in seawater. Geochimica et Cosmochimica Acta, 59 (6) 1063-1071 doi:10.1016/0016-7037(95)00023-s
Saccocia, Peter J, Seyfried, William E (1994) The solubility of chlorite solid solutions in 3.2 wt% NaCl fluids from 300–400°C, 500 bars. Geochimica et Cosmochimica Acta, 58 (2) 567-585 doi:10.1016/0016-7037(94)90489-8
Allen, Douglas E., Seyfried, W.E. (2003) Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: An experimental study at 400°C, 500 bars. Geochimica et Cosmochimica Acta, 67 (8) 1531-1542 doi:10.1016/s0016-7037(02)01173-0
Saccocia, Peter J, Seyfried, William E (1990) Talc-quartz equilibria and the stability of magnesium chloride complexes in NaCl-MgCl2 solutions at 300, 350, and 400°C, 500 bars. Geochimica et Cosmochimica Acta, 54 (12) 3283-3294 doi:10.1016/0016-7037(90)90285-s
Seyfried, W.E. (1984) Hydrothermal processes at Seafloor Spreading Centers. Geochimica et Cosmochimica Acta, 48 (11) 2401 doi:10.1016/0016-7037(84)90242-4
 
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