Continental transverse transform structures (zones) are prevalent features found at various stages of continental evolution and across diverse geodynamic settings. These structures typically manifest as irregularly shaped belts with complex structures, oriented perpendicular or at a high angle oblique to the dominant regional structural trend. There are significant differences in geological characteristics and structural deformation between their two sides. Continental transverse transform structures can be divided into four categories based on their origin, structural characteristics, and associated geological processes: transfer (fault) zones, accommodation (structural) zones, step- over/relay zones, and magmatic- thermal structures. The geological setting and significance of different types and scales of continental transverse transform structures are obviously different. However, there are still many common characteristics among them, such as universality and inconspicuous appearance; features are diverse, complex, and changeable; rupture has shear strike- slip (wrench, rotation) structural characteristics; construction of the same type and class with nearly equidistant distribution. These singuler and common features can be used as clues and a basis for identifying and determining transverse transfer structures. The geological processes associated with the continental transverse transform structures are worthy of attention. They play an important role in transformation, regulation and transforming stress within the continental lithosphere. These structures create distinct zones of deformation and mineralization, contribute to the construction and reformation of geological features, and are often associated with earthquake- prone areas. In terms of mineralization, continental transverse transform structures often manifest as important mineralization belts, causing the zoning of mineral occurrence conditions and reservoir (ore) formation. These significant geological processes, distinctive structural features, and the scale of the transverse transform structures are often closely associated with the time or relative temporal sequence of their development. This article investigates the genesis mechanism of transverse transform structures from three aspects, with a particular focus on the different stages of development, including early pre- existing, synchronous transformation and regulation, and late neogenesis and transformation.