The intercalated shale oil within the first member of the Qingshankou Formation in the southern Songliao Basin exhibits significant exploration potential

primarily influenced by the quality of its intercalations

which impacts both oil content and productivity. The physical properties of these interlayers are notably heterogeneous

highlighting the necessity to characterize and describe interlayer reservoirs comprehe

nsively and establish a suitable classification scheme. This study utilized advanced techniques such as field emission scanning electron microscopy

high-pressure mercury injection

and nuclear magnetic resonance to characterize the reservoir. Employing the fractal theory associated with mercury injection

a physical property classification standard tailored for sandstone interlayers was developed. This standard was combined with logging data to predict the physical property parameters of the reservoirs

facilitating the identification and mapping of high-quality interlayer reservoirs. The results delineate the first member of the Qingshankou Formation in the Daqingzijing area into regions of varying source rock maturity: low maturity areas with a vitrinite reflectance（

R

o

） of less than 1.0% and areas with middle to high maturity source rocks（

R

o

greater than 1.0%）. It was found that interlayer physical properties deteriorate as the maturity of the source rock increases. A grading standard for interlayer physical properties was established

categorizing the sandstone interlayers into Class Ⅰ to Ⅲ

and deeming some as invalid reservoirs. From Class Ⅰ to invalid reservoirs

there is a sequential decrease in the content of large and medium pores

with reservoir space transitioning from intergranular pores and intergranular solution pores to intragranular solution pores and intergranular pores. The mercury injection profiles evolve from weak platforms and slow straight lines to convex shapes

indicating a gradual degradation in oil content. High-quality interlayer reservoirs are predominantly situated along the main body of the estuary bar and the underwater distributary channels

with the thickness decreasing from southwest to northeast. The findings of this research provide crucial insights for targeting interbedded shale oil prospects within the first member of the Qingshankou Formation in the southern Songliao Basin

assisting in the strategic selection of exploration and develop

ment sites.