Illescas Batholith is a geological complex located in Uruguay made up of various plutons including rapakivi granite and quartz syenite. The batholith is of Late Paleoproterozoic age.[1][2] The batholith originated and was emplaced in an anorogenic tectonic setting during a period of extensional tectonics.[2] The batholith intrudes the Valentines Granulitic Complex of Nico Perez Terrane.[2] The Florida dyke swarm is related to the Illescas Batholith.[3]
References
edit- ^ Campal, N., & Schipilov, A. (1999). The eastern edge of the Rio de la Plata Craton: a history of tangential collisions. In Basement Tectonics 13 (pp. 33–48). Springer Netherlands.
- ^ a b c Mallmann, G.; Chemale Jr., F.; Ávila, J.N.; Kawashita, K.; Armstrong, R.A. (2007). "Isotope geochemistry and geochronology of the Nico Pérez Terrane, Rio de la Plata Craton, Uruguay". Gondwana Research. 12 (4): 489–508. Bibcode:2007GondR..12..489M. doi:10.1016/j.gr.2007.01.002.
- ^ Teixeira, Wilson; D'Agrella-Filho, Manoel S.; Hamilton, Mike A.; Ernst, Richard E.; Girardi, Vicente A.V.; Mazzucchelli, Maurizio; Bettencourt, Jorge S. (2013). "U–Pb (ID-TIMS) baddeleyite ages and paleomagnetism of 1.79 and 1.59 Ga tholeiitic dyke swarms, and position of the Rio de la Plata Craton within the Columbia supercontinent". Lithos. 174: 157–174. Bibcode:2013Litho.174..157T. doi:10.1016/j.lithos.2012.09.006.
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