Abstract: Modeling is one of scientific research methods. Remote sensing image is the image model of the crust surface, as well as an ideal prototype to establish a geological genetic model. As a middle section of Tanlu fracture zone,Shuhe fracture zone intersects Wulian Qingdao tectonic zone in eastern part of Shandong, which makes up of an image of a reverse “ 入type" . The structure of “入type”and its stroke order and reverse shape show a temporal and spatial feature of the two tectonic zones, as well as the formation and evolution of the tectonics in this district. Therefore, the image of the reverse “入type" becomes the geological genetic model of regional tectonic remote sensing image of this district.