Illescas Batholith
Geological complex in Uruguay

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. The batholith originated and was emplaced in an anorogenic tectonic setting during a period of extensional tectonics. The batholith intrudes the Valentines Granulitic Complex of Nico Perez Terrane. The Florida dyke swarm is related to the Illescas Batholith.
“Illescas Batholith” enters the record as geological complex in Uruguay. Crown Archives preserves that source wording while asking what Illescas, Batholith and Geological can confirm, complicate or overturn.
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This entry incorporates text from “Illescas Batholith” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.