{"id":155,"date":"2011-12-02T16:10:54","date_gmt":"2011-12-02T16:10:54","guid":{"rendered":"http:\/\/cms.impact-structures.com\/?page_id=155"},"modified":"2012-12-16T12:47:02","modified_gmt":"2012-12-16T12:47:02","slug":"the-ries-impactites","status":"publish","type":"page","link":"http:\/\/estructuras-de-impacto.impact-structures.com\/?page_id=155","title":{"rendered":"LAS IMPACTITAS DE RIES"},"content":{"rendered":"

\"\"LAS IMPACTITAS DE RIES<\/span><\/span><\/p>\n

 <\/p>\n

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Roca de fundido de impacto; procedente de la peque\u00f1a y abandonada cantera de Polsingen. Antiguamente, esta roca de fundido era considerada como una suevita. Puede observarse, no obstante, que la matriz consiste actualmente en un fundido de impacto cristalizado. A diferencia de esta y por definici\u00f3n, una suevita presenta una matriz cl\u00e1stica.<\/span><\/p>\n

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Superf\u00edcie cortada (13 cm de anchura) de la roca de fundido de impacto de Polsingen.<\/p>\n

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Superf\u00edcie cortada (17 cm de anchura) de una brecha suev\u00edtica (procedente de la cantera de Aum\u00fchle).<\/p>\n

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Suevita: variedad de Zipplingen. La anchura de la muestra es de 16 cm.<\/p>\n

\"\"<\/p>\n

Suevita: variedad de Zipplingen. La anchura de la muestra es de 16 cm.<\/p>\n

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Eyecta de la brecha Bunte, cantera de Ronheim. El bloque est\u00e1 compuesto principalmente por lutitas Jur\u00e1sicas y Tri\u00e1sicas, concreciones de caliza fracturadas, y fragmentos de calizas del Malm. La imagen ampliada (debajo) muestra un componente le\u00f1oso transformado parcialmente en carb\u00f3n vegetal y parcialmente en madera petrificada (de color gris\u00e1ceo). La longitud de la llave de coche es de 7 cm.<\/p>\n

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Detalle.<\/p>\n

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Brecha monom\u00edctica de movimiento: granito procedente de la cantera Limberg cerca de Unterwilflingen (ver Afloramientos).<\/p>\n

\"\"\u00a0<\/span><\/p>\n

Brecha monom\u00edctica de movimiento: caliza del Malm procedente de la cantera de Iggenhausen (ver Afloramientos).<\/p>\n","protected":false},"excerpt":{"rendered":"

LAS IMPACTITAS DE RIES   Roca de fundido de impacto; procedente de la peque\u00f1a y abandonada cantera de Polsingen. Antiguamente, esta roca de fundido era considerada como una suevita. Puede observarse, no obstante, que la matriz consiste actualmente en un fundido de impacto cristalizado. A diferencia de esta y por definici\u00f3n, una suevita presenta una … Continuar leyendo \u00abLAS IMPACTITAS DE RIES\u00bb<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":151,"menu_order":2,"comment_status":"closed","ping_status":"closed","template":"sidebar-page.php","meta":{"footnotes":""},"class_list":["post-155","page","type-page","status-publish","hentry"],"yoast_head":"\nLAS IMPACTITAS DE RIES - ERNSTSON CLAUDIN ESTRUCTURAS DE IMPACTO - CR\u00c1TERES METEOR\u00cdTICOS<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"http:\/\/estructuras-de-impacto.impact-structures.com\/?page_id=155\" \/>\n<meta property=\"og:locale\" content=\"es_ES\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"LAS IMPACTITAS DE RIES - ERNSTSON CLAUDIN ESTRUCTURAS DE IMPACTO - CR\u00c1TERES METEOR\u00cdTICOS\" \/>\n<meta property=\"og:description\" content=\"LAS IMPACTITAS DE RIES   Roca de fundido de impacto; procedente de la peque\u00f1a y abandonada cantera de Polsingen. 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