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Quaternary sediments, clay minerals

Besides the clay mineral Ca-montmorillonite, calcite and Fe(OH)2 7Clo.3 also form. All other mineral phases remain dissolved. The hypothesis that there is a hydrochemical influence from the Cretaceous limestone and from the Quaternary sediments because the spring is located above an apparently hydraulically active fault, seems to be correct. The influence of the crystalline basement results from the general groundwater flow from east to west. The model uncertainty is acceptable with 6%. [Pg.159]

See other pages where Quaternary sediments, clay minerals is mentioned: [Pg.44]    [Pg.357]    [Pg.255]    [Pg.352]    [Pg.352]    [Pg.353]    [Pg.217]    [Pg.117]    [Pg.53]    [Pg.368]    [Pg.174]   
See also in sourсe #XX -- [ Pg.352 ]



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Clay minerals

Sediment, mineralization

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