Rocks from Incapillo are rich in sodium and have high ratios of lanthanum and samarium to ytterbium and high ratios of barium to lanthanum, as well as high lead-206 to lead-204 and strontium-87/strontium-86 ratios. These rare-earth element patterns are similar to the Late Miocene Maricunga Belt rocks and contrast to early Miocene rocks. The changes occurred at the same time as the arc migrated eastward, terminating activity in the Maricunga Belt. The element ratios are pronouncedly arc-like with some adakitic signatures. The rocks contain considerably more sodium and alumina than almost all Central Andes siliceous volcanic rocks.