Peraluminous magmas are rare in the Andes but more common in collisionalorogens such the Himalayas. From this it is inferred that the Andean orogeny in Bolivia should have features in common with collisional orogens. This in turn might be related to particularities in the interaction of the South American Plate and the Nazca Plate during the Andean orogeny which led to collision-like events in the Cenozoic at the latitudes of Bolivia. The tectonic mechanism makes the invocation of a long-lived "tin anomaly" beneath the Cordillera Oriental unnecessary.[2]
^ abcMlynarczyk, Michael S.J.; Williams-Jones, Anthony E. (2005). "The role of collisional tectonics in the metallogeny of the Central Andean tin belt". Earth and Planetary Science Letters. 240 (3–4): 656–667. doi:10.1016/j.epsl.2005.09.047.