Article ID Journal Published Year Pages File Type
4727599 Gondwana Research 2012 16 Pages PDF
Abstract
► We have identified late Early Cambrian calk-alkaline metadiorite and MORB-type metapyroxenite in La Pampa (ECIC). ► The ECIC was derived from a juvenile Tonian source, and was intruded into a juvenile late Mesoproterozoic basement. ► The ECIC is located at the tectonic boundary between the Pampia terrane and the Río de la Plata craton.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
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