摘要
Taking the sandbody distribution character of the inner Junggar Basin in Jurassic as an example, this paper discusses the formative mechanism and deformation behavior of high-quality reservoir of structural transfer zones based on the study on the tectonic-sedimentary-diagenesis in structural transfer zones controlling provenances, sand bodys and rock physics and so on. Structural transfer zones control the main provenances and water systems, and then control the development characteristics of the sedimentary systems. Structural transfer zones and slope breaks jointly control the distribution of sedimentary facies. Structural transfer zones, slope breaks and sequence framework control not only the temporal and spatial distribution of sand bodies but also their reservoir qualities. The study on structural transform zones helps to predict reservoirs more accurately and finally provide guidance to the sedimentology of continental lake basins and their exploration and development.