Sequence stratigraphy and depositional pattern of Es4s were documented and discussed.
Sedimentary facies elaborated and described with accordance of characteristic petrological and mineralogical features.
Clastic beach-bar facies (equal or more than 3 m) mainly developed in LST, have good potential towards reservoir.
Carbonate cementation in short high frequency sedimentary cycles and clays affect the reservoir quality significantly.
Interbeds of mud and sand show depositional while cementation and compaction are main causes of diagenetic heterogeneity.