Saergan Formation hydrocarbon source rocks of the Middle-Upper Ordovician are important marine source rocks in the Tarim Basin.Due to the large burial depth of the Middle-Upper Ordovician

a lack of drilling data for horizon calibration in Awati fault depression

and the insignificant seismic response characteristics of hydrocarbon source rocks in the Saergan Formation

it is difficult to accurately predict the distribution of the source rocks with traditional techniques.Based on the analysis of lithology types and stratigraphic configuration in the Saergan Formation together with its overlying and underlying strata on the outcrops in Kalpin area

we established a geologic model for seismic forward modeling.The combination of geological model and seismic model provides a basis for identifying and tracing seismic facies of the source rocks.Following the interpretation of 2D seismic lines one by one in the study area

we analyzed both the seismic and sedimentary facies according to the features of reflection wave groups.As to areas where source rocks occur on the outcrops but are not penetrated by wells emplaced in fault depression

we worked out methods and established the workflow for marine source rock identification

and re-recognized and predicted the spatial distribution of marine source rocks in the Middle-Upper Ordovician Saergan Formation.The results show that the Saergan Formation source rocks

developed under the control of sea level rising

belong to deposits of the deep shelf facies.The Saergan Formation source rocks are widely distributed in the study area with a predicted thickness range of about 0-120 m.It is the thickest in the southwest

thins progressively toward the northeast under the control of the Aqia and Tumuxiuke fault belts

and overlaps to the north till pinches out to the south of Well Yingmai 3;moreover

it still occurs sporadically at the western margin of Aman transitional belt to the east.