The Ordovician Quebrada Grande Formation, Cordón de Lila (Antofagasta Region, northern Chile): stratigraphicand paleogeographic significance
The Cordón de Lila is located immediately to the south of the Salar de Atacama, in northern Chile. The geology of the Cordón de Lila is characterized by extensive outcrops of Early Paleozoic volcanic and sedimentary rocks (Cordón de Lila Igneous and Sedimentary Complex; CISL) that form the 'Arc...
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| Main Authors: | , , , |
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| Language: | English |
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Servicio Nacional de Geología y Minería (SERNAGEOMIN)
2007
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| Online Access: | http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082007000200006 |
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