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词条 Illescas Batholith
释义

  1. References

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

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. ^{{cite journal |last=Mallmann |first=G. |last2=Chemale Jr. |first2=F. |last3=Ávila |first3=J.N. |last4=Kawashita |first4=K. |last5=Armstrong |first5=R.A. |date=2007 |title=Isotope geochemistry and geochronology of the Nico Pérez Terrane, Rio de la Plata Craton, Uruguay |url= |journal=Gondwana Research |publisher= |volume=12 |issue= |pages=489–508 |doi= 10.1016/j.gr.2007.01.002}}
3. ^{{cite journal |last=Teixeira |first=Wilson |last2=D'Agrella-Filho |first2=Manoel S.|last3=Hamilton |first3=Mike A. |last4=Ernst |first4=Richard E. |last5=Girardi |first5=Vicente A.V.|last6=Mazzucchelli |first6=Maurizio|last7=Bettencourt |first7=Jorge S. |date=2013 |title=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 |url= |journal=Lithos |publisher= |volume=174 |issue= |pages=157–174 |doi= 10.1016/j.lithos.2012.09.006}}

4 : Batholiths of South America|Geology of Uruguay|Paleoproterozoic magmatism|Precambrian South America

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