“…1). The Franciscan basement rocks probably evolved near a subduction zone that was later offset, in a right-lateral sense, along a tec tonically "softened" zone between the Pacific and the North American plates (Hamilton, 1969(Hamilton, , 1978Suppe, 1970;Atwater, 1970). The Salinian block was probably derived from between the Mojave block and the Penin sular Range in southern California (Hamilton, 1978;Dickinson, 1983;Ross, 1984) or from the west coast of Mexico and(or) Central America (Howell and others, 1980;Page, 1982).…”