碳酸盐胶结物 （carbonate cement）是指颗粒石灰岩沉积物中的孔隙水过饱和沉淀的碳酸盐矿物。按孔隙水性质及成岩环境的不同，具有不同成分及结构的矿物。
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Carbonate cement occupies lots of pores, it does not favor the preservation of the pore.
碳酸盐胶结物连生胶结占据大量孔隙，不利于孔隙的保存。
The carbonate cement, influenced by the salinity to some degree, is mainly inorganic with few relation to biogas.
碳酸盐主要为无机成因，少量与生物气有关，其含量受盐度的影响。
The main type of carbonate cement was calcite cementing, with little ferrocalcite cement and rare ferrodolomite cement.
碳酸盐胶结的主要类型是方解石胶结，同时也含有少量的铁方解石和极少量的铁白云石胶结。
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