{"id":721,"date":"2013-06-23T23:20:17","date_gmt":"2013-06-23T21:20:17","guid":{"rendered":"https:\/\/ccgm.org\/produit\/carte-geomorphologique-et-tectonique-du-domaine-mediterraneen\/"},"modified":"2025-02-26T20:31:56","modified_gmt":"2025-02-26T19:31:56","slug":"carte-geomorphologique-et-tectonique-du-domaine-mediterraneen","status":"publish","type":"product","link":"https:\/\/ccgm.org\/es\/producto\/mapa-geomorfologico-y-tectonico-del-dominio-mediterraneo\/","title":{"rendered":"Mapa geol\u00f3gico y morfotect\u00f3nico de la zona mediterr\u00e1nea"},"content":{"rendered":"<p><strong>Mapa geol\u00f3gico y morfotect\u00f3nico de la zona mediterr\u00e1nea<\/strong><\/p>\n<p>Tras la publicaci\u00f3n en abril de 2012 de una nueva s\u00edntesis morfobatim\u00e9trica del Mediterr\u00e1neo a escala 1:4.000.000, realizada conjuntamente por Geoazur, el DT-Insu (programa Mistrals) y el Ifremer, en junio de 2012 se public\u00f3 tambi\u00e9n una s\u00edntesis geol\u00f3gica y morfotect\u00f3nica de todo el dominio mediterr\u00e1neo (cuencas marinas y geolog\u00eda circundante) por parte del CCGM.<\/p>\n<p>Esta s\u00edntesis ha sido realizada por J. Mascle (DR CNRS em\u00e9rito, G\u00e9oazur) para el \u00e1mbito marino, y G. Mascle (antiguo profesor de la Universidad J. Fourrier de Grenoble) para el \u00e1mbito peri-mediterr\u00e1neo, con la ayuda del DT-Insu (programa Mistrals).<\/p>\n<p>Construida en un entorno Arcgis, esta recopilaci\u00f3n, la primera publicada a escala de todo el Mediterr\u00e1neo, es el resultado de la superposici\u00f3n de casi treinta capas diferentes que representan otras tantas s\u00edntesis tem\u00e1ticas.<\/p>\n<p><strong>Mapa geol\u00f3gico y morfotect\u00f3nico de la zona mediterr\u00e1nea<\/strong><\/p>\n<p>En tierra, al estar la estructuraci\u00f3n del dominio mediterr\u00e1neo estrechamente vinculada a la evoluci\u00f3n del sistema alpino, los terrenos se agruparon en funci\u00f3n de su participaci\u00f3n en las estructuras alpinas, siendo conscientes de la importancia de la variabilidad temporal y espacial a lo largo de la historia alpina.<\/p>\n<p>En el mar, la s\u00edntesis propuesta tiene en cuenta diversas caracter\u00edsticas de los dominios marinos, como la naturaleza y la edad de las cuencas profundas, la distribuci\u00f3n de las principales cuencas evapor\u00edticas \"mesinianas\", as\u00ed como la de las diversas estructuras (diapiros, tect\u00f3nica sal\u00edfera) resultantes de estos dep\u00f3sitos; tambi\u00e9n se han indicado las principales deformaciones tect\u00f3nicas actuales y\/o recientes, as\u00ed como la distribuci\u00f3n del vulcanismo fangoso y otras salidas de fluidos, a escala de todo el dominio mediterr\u00e1neo. Por \u00faltimo, se ha superpuesto la localizaci\u00f3n de los epicentros de los terremotos (de magnitud superior a 4) en todo el dominio para destacar los l\u00edmites de los principales complejos tect\u00f3nicamente activos, as\u00ed como los l\u00edmites de las placas implicadas.<\/p>\n<p>Las notas y referencias de este mapa pueden descargarse haciendo clic en <a href=\"http:\/\/ccgm.dev.tfs.im\/img\/cms\/Notes%20expl%20morpho-tecto%20web.pdf\" target=\"_blank\" rel=\"noreferrer noopener\">aqu\u00ed<\/a><\/p>\n<p><strong>Mapa geol\u00f3gico y morfotect\u00f3nico de la zona mediterr\u00e1nea<\/strong><\/p>","protected":false},"excerpt":{"rendered":"<p><strong>Mapa geol\u00f3gico y morfotect\u00f3nico de la zona mediterr\u00e1nea<\/strong><\/p>\n<p>Escala 1:4.000.000<br \/>\nSuperficie total: 119 x 85 cm<br \/>\nCCMG \u00a9 2012<br \/>\nAutores: Jean Mascle y Georges Mascle<\/p>\n<p>&nbsp;<\/p>","protected":false},"featured_media":720,"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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