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The proposed mechanism of magma generation in the late Paleozoic and Triassic granitoids is assimilation of crustal material by mantle derived melts, i.e. The isotopic composition of the Paleozoic rocks in the southern Central Andes indicates a coherent evolution of the western Gondwana margin (21–41°S) during the Paleozoic mainly recycling Proterozoic material by sedimentation, metamorphism and magmatism.The magmatism of the Andean cycle represents important additions of juvenile material to the crust.Radiocarbon dating indicates that the marine–lacustrine transition occurred at 8 ka and 8.15 ka, respectively.The correlation of this transition with global sea-level curves allowed the calculation of local uplift rates for the Holocene.36–41 °S) from compositional and isotopic age data of metamorphic and magmatic rocks.The crustal reservoir of this long-standing active continental margin is characterized by the isotopic composition of Paleozoic (meta)sedimentary rocks which is typical of Proterozoic continental crust (Nd model ages 1.6–2.1 Ga; isotopic composition at ca.Chilean territory includes the Pacific islands of Juan Fernández, Salas y Gómez, Desventuradas, and Easter Island in Oceania.Chile also claims about 1,250,000 square kilometres (480,000 sq mi) of Antarctica, although all claims are suspended under the Antarctic Treaty.

The proposed main mechanism of crustal contribution in these rocks is mixing of continent-derived sediments into the mantle wedge.

Southern Chile is rich in forests and grazing lands, and features a string of volcanoes and lakes.

The southern coast is a labyrinth of fjords, inlets, canals, twisting peninsulas, and islands.

The Mesozoic to Tertiary intrusions have a relatively uniform isotopic composition (Pb ca.

37.2–38.4) indicating only small contributions of the crustal reservoir (ca.

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