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Early Non-Marine Diagenesis of Sedimentary Carbonates

A few experiments have been successfully performed at low temperatures to simulate carbonate diagenetic processes for example, cements have been precipitated on skeletal carbonate sands in experimental reaction chambers designed to mimic vadose and phreatic meteoric cementation (Thorstenson et al., 1972 Badiozamani et al., 1977). These cements are remarkably similar in composition and morphology to those found in rocks cemented in the meteoric [Pg.277]

Wherever possible in further analysis of carbonate diagenetic processes, we will consider the diagenetic history of the rocks in light of the framework of plate tectonics. [Pg.280]

See other pages where Early Non-Marine Diagenesis of Sedimentary Carbonates is mentioned: [Pg.277]    [Pg.278]    [Pg.280]    [Pg.282]    [Pg.284]    [Pg.286]    [Pg.288]    [Pg.290]    [Pg.292]    [Pg.294]    [Pg.296]    [Pg.298]    [Pg.300]    [Pg.302]    [Pg.304]    [Pg.306]    [Pg.308]    [Pg.310]    [Pg.312]    [Pg.314]    [Pg.316]    [Pg.318]    [Pg.320]    [Pg.322]    [Pg.324]    [Pg.326]    [Pg.328]    [Pg.330]    [Pg.332]    [Pg.334]    [Pg.336]    [Pg.338]    [Pg.340]    [Pg.342]    [Pg.344]    [Pg.346]    [Pg.348]    [Pg.350]    [Pg.352]    [Pg.354]    [Pg.356]    [Pg.358]    [Pg.360]    [Pg.362]    [Pg.364]    [Pg.366]    [Pg.368]    [Pg.370]   


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Carbon diagenesis

Carbon marine

Carbon sedimentary

Carbonate diagenesis

Carbonate diagenesis marine

Diagenesis

Marine-carbonate

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