{"id":1418,"date":"2011-12-03T13:12:20","date_gmt":"2011-12-03T13:12:20","guid":{"rendered":"http:\/\/cms.impact-structures.com\/?page_id=262"},"modified":"2012-05-26T11:00:43","modified_gmt":"2012-05-26T11:00:43","slug":"topography-and-general-geology-of-the-rubielos-de-la-cerida-structure","status":"publish","type":"page","link":"http:\/\/estructuras-de-impacto.impact-structures.com\/?page_id=1418","title":{"rendered":"Topograf\u00eda y geolog\u00eda general"},"content":{"rendered":"

Topograf\u00eda y geolog\u00eda general de la estructura de\u00a0Rubielos de la C\u00e9rida<\/h2>\n

<\/h2>\n

Las siguientes im\u00e1genes y fotos muestran algunes de las caracter\u00edsticas topogr\u00e1ficas y geol\u00f3gicas generales de Cuenca de impacto elongada de Rubielos de la C\u00e9rida.<\/strong><\/p>\n

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Fig. Delimitaci\u00f3n aproximada de la Cuenca elongada de impacto en la que puede apreciarse el levantamiento central de Rubielos de la C\u00e9rida (CU). \u201cA\u201d indica el eje de la cadena central de levantamientos en continuaci\u00f3n de CU. PM hace referencia al paso de Puerto Minguez donde los afloramientos permiten ver un extenso eyecta de impacto que est\u00e0 descrito en un cap\u00edtulo aparte (ver eyectas de impacto). T se\u00f1ala el anillo de Torrecilla que es posiblemente una estructura de impacto acompa\u00f1ante del gran evento de impacto m\u00faltiple de Azuara. Teruel es la capital de la provincia as\u00ed denominada. La parte este de la cuenca de impacto est\u00e1 parcialmente ocultada por los sedimentos m\u00e1s j\u00f3venes post-impacto del Terciario.<\/p>\n

\"Image004\"<\/p>\n

Fig. 2. Parte norte final de la cadena central de levantamientos que emerge a trav\u00e9s del cuaternario de la cuenca de impacto elongada (colores claros). Google Earth.<\/p>\n

\"Image006\"<\/p>\n

Fig. 3. Borde oeste de la cuenca de impacto vista desde la cadena central de levantamientos cerca de Torrelac\u00e1rcel. \"Image008\"<\/p>\n

 <\/p>\n

Fig. 4. Borde sur de la cuenca de impacto (al fondo) visto desde la parte sur final de la cadena central de levantamientos (en primer plano) cerca de Concud.<\/p>\n

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Fig. 5.\u00a0Parte de la cadena de levantamientos centrales sobresaliendo del cuaternario de la cuenca de impacto (continuaci\u00f3n del levantamiento central de Rubielos de la C\u00e9rida hacia el sur; v\u00e9ase Fig. 1)<\/span><\/p>\n

\"Image012\"<\/p>\n

Fig. 6. Detalle de la cadena central de levantamientos (sierra Palomera) que muestra capas de rocas carbonatadas del Jur\u00e1sico con buzamientos muy inclinados.<\/p>\n

\"Image014\"<\/p>\n

Fig. 7.\u00a0Mapa geol\u00f3gico general de la parte norte de la cuenca de impacto de Rubielos de la C\u00e9rida (inicialmente: estructura de impacto de Rubielos de la C\u00e9rida), donde se destaca sobretodo el levantamiento central.<\/span><\/p>\n

\"Image016\"<\/p>\n

Fig. 8.\u00a0Corte geol\u00f3gico del levantamiento central de Rubielos de la C\u00e9rida.<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"

Topograf\u00eda y geolog\u00eda general de la estructura de\u00a0Rubielos de la C\u00e9rida Las siguientes im\u00e1genes y fotos muestran algunes de las caracter\u00edsticas topogr\u00e1ficas y geol\u00f3gicas generales de Cuenca de impacto elongada de Rubielos de la C\u00e9rida. Fig. Delimitaci\u00f3n aproximada de la Cuenca elongada de impacto en la que puede apreciarse el levantamiento central de Rubielos de … Continuar leyendo \u00abTopograf\u00eda y geolog\u00eda general\u00bb<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":1417,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"sidebar-page.php","meta":{"footnotes":""},"class_list":["post-1418","page","type-page","status-publish","hentry"],"yoast_head":"\nTopograf\u00eda y geolog\u00eda general - 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=1418\" \/>\n<meta property=\"og:locale\" content=\"es_ES\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Topograf\u00eda y geolog\u00eda general - ERNSTSON CLAUDIN ESTRUCTURAS DE IMPACTO - CR\u00c1TERES METEOR\u00cdTICOS\" \/>\n<meta property=\"og:description\" content=\"Topograf\u00eda y geolog\u00eda general de la estructura de\u00a0Rubielos de la C\u00e9rida Las siguientes im\u00e1genes y fotos muestran algunes de las caracter\u00edsticas topogr\u00e1ficas y geol\u00f3gicas generales de Cuenca de impacto elongada de Rubielos de la C\u00e9rida. 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