About the sedimentary facies of the Jia 2 Member,Jialingjiang Formation,Lower Triassic in Centre Sichuan,there exists a disagreement on tidalflat
deposition and nontidalflat deposition for many years.On the basis of fine core description,thinsection identification and logging analysis,according to the
analysis of sedimentary characteristics,such as sedimentary palaeogeographic background,lithology,sedimentary structures,sedimentary rhyme,palaeoclimate and digenetic
evolution,it is realized that tidal flat facies is not widly distributed in Jia 2 Member,Moxi gas field,but the restricted to evaporate carbonate platform facies in the
epeiric sea is common,and subtidal reducing environment is dominant.The depositional characteristics of similar tidalflat environment exist in the Jia22 B bed
only.It is recognized that the sedimentary facies in Jia 2 Member mainly include platform flat,grain shoal,interbank sea,semirestricted to restricted lagoon,
evaporative lagoon subfacies and so on.The Jia 21 Submember is mainly composed of the deposition of semirestricted to restricted to evaporate lagoon and
interbedded tempestite.The Jia 22 A Bed is characterized by the development of oolitic shoal microfacies.The Jia 22 B Bed is featured by the development of platform
flat subfacies.The sandsize intraclast shoal and evaporative lagoon subfacies are developed in the Jia 22 C Bed.By the analysis of a change of reservoir
porosity with microfacies,it is shown that the dolomite flat,sandsize intraclast shoal and oolitic shoal are favorable reservoir microfacies.