Peperita (roca) Referencias Menú de navegaciónSkilling, I.P., White, J.D.L/ & McPhie, J. 2002....


Rocas siliciclásticasRocas volcanosedimentarias


roca sedimentariarocas ígneaslavaLimañaFrancia











Peperita
Tipo
Sedimetaria—Clástica
[editar datos en Wikidata]

La peperita es una roca sedimentaria compuesta de fragmentos de rocas ígneas que se originan al entrar lava en contacto con sedimentos húmedos.[1]​ El término se utilizó originalmente para describir a una roca de la región de Limaña en Francia.[2]​



Referencias




  1. ↑ Skilling, I.P., White, J.D.L/ & McPhie, J. 2002. Peperite: a review of magma-sediment mingling, Journal of Volcanology and Geothermal Research, 114, 1-17


  2. ↑ de Goer de Herve, A. 2008. Chapter 5, Peperites from the Limagne Trench (Auvergne, French Massif Central), a distinctive feature of phreatomagmatic pyroclastics. History of semantic drift. In: Leyrit, H. & Montenat, C. (Eds.) Volcaniclastic rocks, from magmas to sediments, Taylor & Francis, 270pp.







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