{"id":706,"date":"2013-06-23T22:53:54","date_gmt":"2013-06-23T20:53:54","guid":{"rendered":"https:\/\/ccgm.org\/produit\/carte-structurale-de-l-ocean-atlantique\/"},"modified":"2024-04-09T22:56:11","modified_gmt":"2024-04-09T20:56:11","slug":"carte-structurale-de-locean-atlantique","status":"publish","type":"product","link":"https:\/\/ccgm.org\/es\/producto\/mapa-estructural-del-oceano-atlantico-2\/","title":{"rendered":"Mapa estructural del Oc\u00e9ano Atl\u00e1ntico"},"content":{"rendered":"<p><strong>Mapa estructural del Oc\u00e9ano Atl\u00e1ntico<\/strong><\/p>\n<p>Este mapa, que abarca todo el Oc\u00e9ano Atl\u00e1ntico, se publica con motivo del 34\u00ba Congreso Geol\u00f3gico Internacional (Brisbane, agosto de 2012) y es una ampliaci\u00f3n del Mapa Estructural del Atl\u00e1ntico Norte (2008), al que sustituye. Sintetiza las interpretaciones geol\u00f3gicas y los datos geof\u00edsicos, que abarcan varias d\u00e9cadas, recopilados de campa\u00f1as en alta mar y de las publicaciones resultantes.<\/p>\n<p>El mapa principal, estructural, muestra el oc\u00e9ano y los continentes circundantes con sus caracter\u00edsticas estructurales simplificadas. Los siguientes elementos est\u00e1n representados en el dominio oce\u00e1nico:<\/p>\n<p>- Edad de la corteza oce\u00e1nica, por \u00e9pocas<br \/>\n- Posiciones de anomal\u00edas magn\u00e9ticas est\u00e1ndar (o \"crono\"), donde se hayan medido o interpretado<br \/>\n- Ejes de expansi\u00f3n oce\u00e1nica, activos y f\u00f3siles<br \/>\n- Fallas de transformaci\u00f3n y zonas de fractura<br \/>\n- Rasgos submarinos \"an\u00f3malos\" y zonas de subducci\u00f3n<br \/>\n- Secuencias de reflectores inclinados oce\u00e1nicos (SDR)<br \/>\n- Epicentro del terremoto y profundidad del foco<br \/>\n- Puntos calientes<br \/>\n- Lugares de perforaci\u00f3n oce\u00e1nica profunda (DSDP, IPOD, ODP, IODP) donde se ha alcanzado el lecho rocoso o la corteza de transici\u00f3n<br \/>\n- Espesor de los sedimentos, con isopaques dibujados en la corteza oce\u00e1nica o en zonas de corteza continental adelgazada.<br \/>\n- Zonas de deformaci\u00f3n de la corteza oce\u00e1nica<br \/>\n- Representaci\u00f3n de los elementos de geolog\u00eda continental relacionados con la apertura del oc\u00e9ano Atl\u00e1ntico<\/p>\n<p>Mapa estructural del Oc\u00e9ano Atl\u00e1ntico<\/p>\n<p>El mapa estructural va acompa\u00f1ado de un Esquema Geodin\u00e1mico (como inserto en el mapa y descargable haciendo clic en <a href=\"http:\/\/ccgm.dev.tfs.im\/img\/cms\/Physio%20A3%20milieu%20%20notes.jpg\" target=\"_blank\" rel=\"noreferrer noopener\">aqu\u00ed<\/a>) y un Mapa Fisiogr\u00e1fico (insertado en el centro de las notas explicativas que puedes descargar haciendo clic en <a href=\"http:\/\/ccgm.dev.tfs.im\/img\/cms\/Notes%20Atlant%20UK-FR_final.pdf\" target=\"_blank\" rel=\"noreferrer noopener\">aqu\u00ed<\/a>). Estos dos documentos muestran la disposici\u00f3n de las placas litosf\u00e9ricas que cubren o encierran el dominio atl\u00e1ntico, la morfolog\u00eda del conjunto, as\u00ed como la toponimia de cierto n\u00famero de estructuras submarinas mencionadas en el texto.<\/p>\n<p>El mapa ha contado con el apoyo financiero de la UNESCO, el Servicio Geol\u00f3gico de Noruega (2008) y el IFREMER (Francia).<\/p>\n<p>Mapa estructural del Oc\u00e9ano Atl\u00e1ntico<\/p>","protected":false},"excerpt":{"rendered":"<p><strong>Mapa estructural del Oc\u00e9ano Atl\u00e1ntico<\/strong><\/p>\n<p>Escala ecuatorial: 1:20 000 000<br \/>\nPublicado en julio de 2012<br \/>\n1 hoja: 119 x 84 cm<br \/>\nCCGM-CGMW 2012<\/p>\n<p>Autor: Peter S. Miles (CCMG)<br \/>\nCoautores: Philippe Bouysse (CCGM) y Kaiser de Souza (CPRM, Brasil)<\/p>","protected":false},"featured_media":705,"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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}}},"product_cat":[59,54,64,61],"product_tag":[414,417,419,421,422,418,415,416,420],"_links":{"self":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/706"}],"collection":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product"}],"about":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/types\/product"}],"replies":[{"embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/comments?post=706"}],"version-history":[{"count":0,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/706\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media\/705"}],"wp:attachment":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media?parent=706"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_cat?post=706"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_tag?post=706"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}