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Burial diagenesis original composition

Many chalks undergoing burial diagenesis in the present oceanic realm and those exposed on land were originally pelagic foram-nannofossil calcite oozes. However, calcareous oozes deposited in the periplatform environment are compositionally more complex. These oozes represent transitional carbonate deposits found between carbonate banks and the deep sea (Schlager and James,... [Pg.408]

See other pages where Burial diagenesis original composition is mentioned: [Pg.411]    [Pg.386]    [Pg.363]    [Pg.412]    [Pg.424]    [Pg.53]    [Pg.183]    [Pg.184]    [Pg.19]    [Pg.442]    [Pg.442]    [Pg.717]    [Pg.9]    [Pg.62]    [Pg.345]    [Pg.470]    [Pg.269]   
See also in sourсe #XX -- [ Pg.408 , Pg.409 , Pg.410 ]



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