Dyke swarms of Tandil and Azul

The dyke swarms of Tandil and Azul are groups of dykes of Proterozoic age located in Buenos Aires Province, Argentina. The dyke swarms consists of two groups: 2000 million year old dykes of calc-alkaline type and 1600 million year old dykes of tholeiitic type.[1] The tholeiitic dykes are made up of diabase and titanium-rich basalt, in contrast the calc-alkaline dykes are made up of andesite and rhyolite.[2] The dyke swarms intrude the southern part of the Río de la Plata Craton, much the same way the Uruguayan dyke swarms intrude the northeastern part of the craton.[1] The calc-alkaline dykes intruded during a period of transtensional tectonics during the Transamazonian Orogeny while the tholeiitic dykes intruded during the period of extensional tectonics that succeeded the orogeny.[1]

References

  1. 1 2 3 Iacumin, M.; Piccirillo, E.M.; Girardi, V.A.V.; Teixeira, W.; Bellieni, G.; Echeveste, H.; Fernández, R.; Pinese, J.P.P.; Ribot, A. (2001). "Early proterozoic calc-alkaline and middle proterozoic tholeiitic Dyke Swarms from Central–Eastern Argentina: petrology, geochemistry, Sr–Nd isotopes and tectonic implications". Journal of Petrology. 42 (11): 2109–2143.
  2. ↑ Lajoinie, M.F.; Etcheverry, R.O; Lanfranchini, M.E.; Cábana, C. (2014). "Geología, geoquímica y génesis de diques proterozoicos del área de San Miguel, sierras septentrionales de la provincia de Buenos Aires.". Revista de la Asociación Geológica Argentina (in Spanish). 71 (3): 404–415.
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.