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Lopolito Referencias Bibliografía Menú de navegación«Rocas y yacimientos ortomagmáticos»«Lacolitos»«Rocas Ígneas»Léxico de geología económica

Multi tool use
Multi tool use

Cuerpos intrusivos


intrusiónmagmáticaFrank Fitch Grout1918gabroDuluthestratosyacimientos mineralesplatinoidescromoníquelcomplejo de BushveldSudáfricacomplejo de SudburyCanadá












Lopolito




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Representación gráfica de distintos tipos de intrusiones: 1, Lacolito. 2, Dique pequeño. 3, Batolito. 4, Dique. 5, Lámina. 6, Cuello volcánico. 7, Lopolito.


Un lopolito es una intrusión magmática lenticular con forma de cubeta.[1]​ El primero en emplear este término fue Frank Fitch Grout en el año 1918 al describir la intrusión de gabro de Duluth.[2]​ Este cuerpo intrusivo no corta a los estratos encajantes, por lo que se le considera un cuerpo intrusivo concordante.[3]​ Muchos yacimientos minerales de platinoides, cromo (Cr) y níquel (Ni) se asocian a los lopolitos, como el complejo de Bushveld (Sudáfrica), o el complejo de Sudbury (Canadá).[4]​



Referencias



  1. ↑ Higueras, Pablo. «Rocas y yacimientos ortomagmáticos». Universidad de Castilla-La Mancha. Consultado el 2 de septiembre de 2011. 


  2. ↑ Instituto Superior de Correlación Geológica. «Lacolitos». Consultado el 2 de septiembre de 2011. 


  3. ↑ Petróleos de Venezuela SA. «Rocas Ígneas». Consultado el 2 de septiembre de 2011. 


  4. ↑ (Oyarzún M., 2009, p. 47)



Bibliografía



  • Oyarzún M., Jorge (2009). Léxico de geología económica. Madrid, ES. Universidad Complutense de Madrid. p. 81. 



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