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Diagenetic and porosity evolution of conglomerate sandstones in聽Bayingebi Formation of the Lower Cretaceous, Chagan Sag, China-Mongolia frontier area
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文摘

Quantitative diagenesis in the conglomerate sandstones was examined.

Porosity and permeability reduction were caused by compaction and cementation.

Clays and carbonate cements in conglomerate sandstones reduced reservoir quality.

Dissolution of carbonate cement and metastable framework grains caused high porosity.

Thickly bedded channels (>2 m) of fan delta front have high porosity.

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