Abstract
The coastal range of Chile between 36° and 41 °S (Fig. 1) is mainly composed of low-grade metamorphic rocks developed in a subduction-accretion environment during Paleozoic times.
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References
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Hervé, F. et al. (1990). Rb-Sr and Sm-Nd Data from Some Massive Sulfide Occurrences in the Metamorphic Basement of South-Central Chile. In: Fontboté, L., Amstutz, G.C., Cardozo, M., Cedillo, E., Frutos, J. (eds) Stratabound Ore Deposits in the Andes. Special Publication No. 8 of the Society for Geology Applied to Mineral Deposits, vol 8. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-88282-1_16
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