Triple junctions involve the movement of three tectonic plates, and therefore represent one of the most challenging settings to understand deformation processes (e.g., Kleinrock & Morgan, 1988;McKenzie & Morgan, 1969;Patriat & Courtillot, 1984). McKenzie and Morgan (1969) identified 16 possible cases of triple junctions, among which the only stable case for all velocity conditions is the extensional Ridge-Ridge-Ridge triple junction (RRR), in which the three plates move away from each other. For this reason, RRR junctions can be preserved independent of the individual extension directions, and therefore they may exhibit symmetrical settings (with rift branches at 120°) as well as extremely asymmetric geometries.