Abstract
In this paper, through rock core, logging curve, plane shape, distribution and other characteristics in the research area, combined with regional data, the Permo-Carboniferous Strata in the research area experienced tidal flat sedimentary system, delta sedimentary system and river sedimentary system, flood-overlake sedimentary system from bottom to top, it is proved that basin filling evolution of the epicontinental sea basin from occurrence, development to extinction.
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