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《Journal of Chengdu University of Technology(Science & Technology Edition)》 1986-04
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CEMENTATION OF CARBONATE SEDIMENTS

Zhang Changjun  
The diagenetic environment of cementation of carbonate sediments canbe different from the sedimentary environment, for instance, sedimentsbelow sea level can be lifted up above sea level and cemented there.Properties of cementation material, therefore, can be used for identificationof sedimentary and diagenetic environments. Among sedimentaryenvironments, deep sea, shallow sea, subtidal zone, intratidal zone,supratidal zone, Sabkha, reef and beach are recognized. Fromdiagenetic environments, Supratidal Zone, freshwater vadose zone, phreaticzone and burrial zone are descriminated. The main cementation types offreshwater diagenesis are meniscus, pendaet, infiltrated sand, co-axialgrowth and freshwater equannt calcite and so on. The well developeddissolved pores in these types of cement are especially good for oil-gastrap and mineralization of metal resources,
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