Illescas Batholith

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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]

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The Superior Craton is a stable crustal block covering Quebec, Ontario, and southeast Manitoba in Canada, and northern Minnesota in the United States. It is the biggest craton among those formed during the Archean period. A craton is a large part of the Earth's crust that has been stable and subjected to very little geological changes over a long time. The size of Superior Craton is about 1,572,000 km2. The craton underwent a series of events from 4.3 to 2.57 Ga. These events included the growth, drifting and deformation of both oceanic and continental crusts.

References

  1. 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.
  2. 1 2 3 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. doi:10.1016/j.gr.2007.01.002.
  3. 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. doi:10.1016/j.lithos.2012.09.006.