Crystalline dolostone is formed by seepage - reflux dolomitization and burial dolomitization.
晶粒白云巖有兩種成因:一為回流滲透白云石化;二為深埋藏白云石化.
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The diageneses which are constructive to the reservoirs are mainly dolomitization and burial dissolution.
對儲層起建設性作用的成巖作用主要有白云石化作用、埋藏溶解作用.
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The dolomitization is dominated by mixed water dolomitization in the diagenetic stage, followed by burial dolomitization.
白云石化作用,以早成巖階段混合水白云石化作用為主, 埋藏白云石化作用次之.
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