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Diagenesis and origin of calcite cement in the Flemish Pass Basin sandstone reservoir (Upper Jurassic): Implications for porosity development
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文摘

Petrographic characteristics and diagenesis evolution of Ti-3 sandstones.

Early formed calcite cement was sourced from the dissolution of biogenic marine carbonates in the modified seawaters evidenced by bulk geochemical data.

The maturation of organic matters played a significant role in the porosity improvement.

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