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Cherts y otras rocas de la sílice formadas por reemplazamiento: indicadores estables de ambientes diagenéticos.

AuthorsBustillo, Mª Ángeles
Issue Date28-Sep-1999
PublisherUniversidad de Salamanca
CitationEN: Dinámica de las interacciones entre agua y minerales en medios de baja temperatura (meteorización , diagénesis, metasomatismo), 103-109
AbstractInorganic cherts and opals, formed by diagenetic silicification, appear in a wide variety of rocks and they are testimony of the replacement environments. Textures and structures of the host rocks, during the silicification, remain in the cherts and opals when the replacement is isovolumetric and some examples of these cases are discussed. The main silica minerals and textures are described considering the general genetic conditions of formation and the lithology of the replaced host rock. Several general pattems, in relation to these subjects, are explained considering that when these pattems are not found, special conditions must be considered.
DescriptionConferencia en una Reunión Científica
Appears in Collections:(MNCN) Comunicaciones congresos
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