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Carbonate dissolution mesogenetic

The origin of widely variable, but generally low 6 values of both mesogenetic calcite and dolomite is poorly constrained, but could be related to C derivation from several sources, such as soil CO2 in modified meteoric waters, the dissolution of eogenetic carbonates and thermal decarboxylation of organic matter. As there is no correlation between 6 C and 6 0 values (Fig. 10), the input of carbon has not been related to temperature or to progressive, systematic variations in fl uid composition. [Pg.134]

Mazzullo SJ, Harris PM (1992) Mesogenetic dissolution its role in porosity development in carbonate reservoirs. Am Assoc Pet Geol Bull 76 607-620 Menaul PL (1944) Causative agents of corrosion in distillate field. Oil Gas J, Nov 11 ... [Pg.112]


See other pages where Carbonate dissolution mesogenetic is mentioned: [Pg.13]    [Pg.1]    [Pg.13]    [Pg.18]    [Pg.53]    [Pg.74]    [Pg.107]    [Pg.137]   
See also in sourсe #XX -- [ Pg.13 ]




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