{"id":820,"date":"2013-12-19T18:33:21","date_gmt":"2013-12-19T17:33:21","guid":{"rendered":"https:\/\/ccgm.org\/produit\/carte-structurale-de-la-plaque-arabie-et-regions-avoisinantes\/"},"modified":"2024-05-15T15:15:49","modified_gmt":"2024-05-15T13:15:49","slug":"carte-structurale-de-la-plaque-arabie-et-regions-avoisinantes","status":"publish","type":"product","link":"https:\/\/ccgm.org\/es\/producto\/mapa-estructural-del-plano-arabe-y-las-regiones-vecinas\/","title":{"rendered":"Mapa estructural de la Placa Ar\u00e1biga y sus alrededores"},"content":{"rendered":"<p><strong>Mapa estructural de la Placa Ar\u00e1biga y sus alrededores<\/strong><\/p>\n<p class=\"MsoNormal\" style=\"margin-bottom: 0.0001pt; line-height: normal;\">El <strong><em>Mapa estructural de la placa ar\u00e1biga<\/em><\/strong> <strong><em>y zonas aleda\u00f1as<\/em><\/strong> ha sido apoyada por el GCCC con el objetivo de tender puentes entre la <em>Mapa tect\u00f3nico de \u00c1frica<\/em> (publicado en 2010) y el <em>Mapa tect\u00f3nico internacional de Asia<\/em> (en curso), y tambi\u00e9n por la importancia de la Placa \u00c1rabe para comprender los procesos geodin\u00e1micos que condujeron a la colisi\u00f3n entre los bloques africano y euroasi\u00e1tico.<\/p>\n<p>&nbsp;<\/p>\n<p class=\"MsoNormal\" style=\"margin-bottom: 0.0001pt; line-height: normal;\">La realizaci\u00f3n de este <strong>Mapa estructural de la Placa Ar\u00e1biga y sus alrededores<\/strong> se realiz\u00f3 en el marco de los acuerdos de investigaci\u00f3n establecidos entre la empresa TOTAL, la Universidad de Cergy-Pontoise y el CCGM.  Es el resultado de una s\u00edntesis de un gran n\u00famero de contribuciones internacionales y de datos publicados e in\u00e9ditos.<\/p>\n<p>&nbsp;<\/p>\n<p class=\"MsoNormal\" style=\"margin-bottom: 0.0001pt; line-height: normal;\">El mapa se centra en la evoluci\u00f3n Fanerozoica. Por tanto, no se diferencian los afloramientos del basamento panafricano en los escudos ar\u00e1bigo y nubio.  En el basamento, el espesor de los dominios d\u00e9bilmente deformados (cuencas intracontinentales, m\u00e1rgenes continentales) se ha representado mediante isopaques.<\/p>\n<p>&nbsp;<\/p>\n<p class=\"MsoNormal\" style=\"margin-bottom: 0.0001pt; line-height: normal;\">Cuando es posible (Plataforma Ar\u00e1biga), se muestran dos series de isopaques por encima y por debajo de las discordancias paleozoicas m\u00e1s importantes bajo las formaciones del Carbon\u00edfero Superior.  En los sistemas orog\u00e9nicos que unen la Plataforma Ar\u00e1biga con el norte (cordilleras de Zagros, Makran y Om\u00e1n), la edad de las principales deformaciones se muestra en color.  En la regi\u00f3n de los Zagros, esta representaci\u00f3n muestra la propagaci\u00f3n de la deformaci\u00f3n desde la sutura hasta la cadena anterior, as\u00ed como el frente de deformaci\u00f3n actual.<\/p>\n<p class=\"MsoNormal\" style=\"margin-bottom: 0.0001pt; line-height: normal;\">Se muestran una serie de bloques continentales entre la sutura de Zagros y los afloramientos indiferenciados del dominio euroasi\u00e1tico en la esquina NE del mapa. Se distinguen dos categor\u00edas, los bloques Cimerios al este y los bloques Tauro-Armenios al oeste. Tambi\u00e9n se indican claramente las suturas principales a lo largo de los l\u00edmites de las placas principales y las suturas menores en los dominios Cimerio y Tauro-Armenio.<\/p>\n<p><strong>Mapa estructural de la Placa Ar\u00e1biga y sus alrededores<\/strong><\/p>","protected":false},"excerpt":{"rendered":"<p><strong>Mapa estructural de la Placa Ar\u00e1biga y sus alrededores<\/strong><\/p>\n<p>Escala ca. 1\/4 600 000<br \/>\nPublicado en 2013<br \/>\nTama\u00f1o de cada tarjeta: 126 cm x 89 cm<br \/>\nCCMG \u00a9 2013<br \/>\nAutores: Dominique Frizon de Lamotte y Pascale Leturmy<\/p>","protected":false},"featured_media":819,"comment_status":"closed","ping_status":"closed","template":"","meta":{"inline_featured_image":false,"site-sidebar-layout":"default","site-content-layout":"default","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"default","adv-header-id-meta":"","stick-header-meta":"default","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"set","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center 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