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Water, acid magmatic

Garrels and Mackenzie (1974) report that as the crust solidified and magmatic minerals crystallized, volatile gases were liberated, forming the atmosphere. Below 100°C all the H2O would have condensed and all acid gases would have reacted with the primordial crust. In the first version, at 600°C the atmosphere would have had a Ph o 300 atm (it corresponds to the mass of water on the present oceans), Pqq 45 atm (it corresponds to... [Pg.49]

See other pages where Water, acid magmatic is mentioned: [Pg.81]    [Pg.113]    [Pg.261]    [Pg.262]    [Pg.1689]    [Pg.1690]    [Pg.103]    [Pg.68]    [Pg.192]    [Pg.188]    [Pg.470]    [Pg.238]    [Pg.264]    [Pg.279]   
See also in sourсe #XX -- [ Pg.154 ]



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