通过对岩心沉积物间隙水成分的研究，表明成岩环境主要为还原环境。
The study on the composition of interstitial water in the sediment shows that diagenesis environment is mainly a reductive environment.
储层的物性主要受沉积物原始组分、沉积作用、成岩作用和构造作用的多重影响。
The physical properties of reservoir are mainly affected by the multi-effects of the original composition of sediments, sedimentation, diagenesis and tectonism.
蒸发岩、风成沉积物以及潮泛沉积物都是常见于潮上盐难的。
Evaporites, eolian deposits and tidal-flood deposits are common in sabkhas.
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