Basins strike-slip

Lallemand and Jolivet (1986) have interpreted the opening of the Japan Sea as a pull-apart basin between two right-lateral strike-slip fault zones the Yagsan-Tsushima fault to the west and the Tartary-Hidaka shear zone to the east. 

The volcanoes of the Roman Province developed in a region characterised by Late Miocene-Quaternary extensional tectonics related to the eastward migration of Apennine mountain range and to the contemporaneous opening of the Tyrrhenian Sea. The volcanic zone is characterised by a system of Upper Miocene to Pleistocene NW-SE basins, developed along normal faults and intersected by strike-slip NE-SW faults (Bartolini et al. 1982). Both fault systems represent zones of crustal weakness along which Roman potassic magmas were intruded. 

C. Hinterland foreland, strike-slip, and graben basins (on overriding plate)... 

Krapez, B. Barley, M. E. 1987. Archaean strike-slip faulting and related ensialic basins evidence from the Pilbara Block, Australia. Geological Magazine, 124, 555-567. 

Crustal thinning by extensional tectonics, causing fault-controlled subsidence (e.g. rift basins like the North Sea, and strike-slip basins as formed along the San Andreas fault zone). 

Active continental margin — Andean- pe basins developed on or adjacent to thick continental margins. Strike-slip basins also develop in this environment... 

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