{"id":10289,"date":"2023-03-23T12:23:04","date_gmt":"2023-03-23T11:23:04","guid":{"rendered":"https:\/\/ccgm.org\/?post_type=product&p=10289"},"modified":"2025-02-27T13:05:59","modified_gmt":"2025-02-27T12:05:59","slug":"tectonics-of-the-antarctic-pdf","status":"publish","type":"product","link":"https:\/\/ccgm.org\/es\/producto\/tectonics-of-the-antarctic-pdf\/","title":{"rendered":"Tect\u00f3nica de la Ant\u00e1rtida-PDF"},"content":{"rendered":"

Tect\u00f3nica de la Ant\u00e1rtida-PDF<\/strong><\/p>\n

La 1\u00aa edici\u00f3n del mapa tect\u00f3nico de la Ant\u00e1rtida a escala 1:10 M<\/a> fue publicada por el CGPC en 2012.<\/p>\n

La importante afluencia de nuevos datos en la \u00faltima d\u00e9cada ha impulsado la actualizaci\u00f3n del mapa de 2012 y la preparaci\u00f3n de la 2\u00aa edici\u00f3n.<\/p>\n

El dise\u00f1o de la leyenda proporciona una presentaci\u00f3n visual compacta de la informaci\u00f3n geodin\u00e1mica y relacionada con la edad. Las unidades cartogr\u00e1ficas se distinguen principalmente por el tipo de corteza que representan y por su formaci\u00f3n en los l\u00edmites de placas o en entornos intraplaca.<\/p>\n

La corteza oce\u00e1nica se cartograf\u00eda seg\u00fan la edad identificada por las anomal\u00edas magn\u00e9ticas. Los complejos arqueanos se agrupan en un bloque separado en la leyenda, que se supone representa una primitiva infraestructura plut\u00f3nica\/metam\u00f3rfica continental (protocostra) desprovista de marcadores claros de tect\u00f3nica de placas.<\/p>\n

Los complejos proterozoicos y fanerozoicos se conocen como terranos continentales no estirados o estirados.<\/p>\n

La corteza no estirada incluye los cinturones de pliegues de acreci\u00f3n (or\u00f3genos), los productos estructurales de su reelaboraci\u00f3n, las cubiertas de las plataformas y los sistemas de pliegues intraplaca.<\/p>\n

La corteza continental estirada controla la distribuci\u00f3n de los sistemas de rift y las cuencas sedimentarias asociadas. Gran parte del margen continental ant\u00e1rtico es rico en magma. En largas zonas adyacentes a la corteza oce\u00e1nica, la corteza continental est\u00e1 hiperestirada, hasta el punto de dejar al descubierto el manto superior.<\/p>\n

Una vista general de las estructuras tect\u00f3nicas ant\u00e1rticas, incluida su distribuci\u00f3n inferida bajo la capa de hielo, se ofrece en un recuadro a menor escala que tambi\u00e9n muestra las tasas de extensi\u00f3n del fondo marino y las zonas de corteza oce\u00e1nica engrosada.<\/p>\n

Tect\u00f3nica de la Ant\u00e1rtida-PDF<\/strong><\/p>","protected":false},"excerpt":{"rendered":"

Tect\u00f3nica de la Ant\u00e1rtida-PDF<\/strong><\/p>\n

Notas explicativas del \"Mapa Tect\u00f3nico de la Ant\u00e1rtida\", escala 1:10 000 000, segunda edici\u00f3n<\/p>\n

Versi\u00f3n digital .pdf de alta resoluci\u00f3n descargable<\/strong><\/p>\n

Nota: Este producto est\u00e1 sujeto a un acuerdo de licencia.<\/strong><\/p>\n

Autores : Garrik Grikurov & German Leitchenkov
\r\nEditor: CCGM-CGMW
Presidente: M. Pubellier\r\nPresidente: M. Pubellier, Secretario General: P. Nehlig, Vicesecretario General: N. Ellouz-Zimmermann, ex presidente: P. Rossi
\r\nComposici\u00f3n y dise\u00f1o: C. Fran\u00e7ois<\/p>\n

Versi\u00f3n inglesa.<\/p>","protected":false},"featured_media":13115,"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":[59,768,54,767,62,71,55,56],"product_tag":[327,405,406],"class_list":{"0":"post-10289","1":"product","2":"type-product","3":"status-publish","4":"has-post-thumbnail","6":"product_cat-tous-nos-produits","7":"product_cat-zones-polaires","8":"product_cat-cartes","9":"product_cat-grandes-regions-du-monde","10":"product_cat-continents","11":"product_cat-antarctique","12":"product_cat-versions-numeriques-des-cartes-et-livrets","13":"product_cat-livrets","14":"product_tag-antarctique","15":"product_tag-tectonique-de-lantarctique","16":"product_tag-tectonique-regions-polaires","17":"product_shipping_class-enveloppe","18":"desktop-align-left","19":"tablet-align-left","20":"mobile-align-left","21":"ast-product-gallery-layout-horizontal-slider","22":"ast-product-gallery-with-no-image","23":"ast-product-tabs-layout-distributed","25":"first","26":"instock","27":"downloadable","28":"virtual","29":"purchasable","30":"product-type-simple"},"_links":{"self":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/10289"}],"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=10289"}],"version-history":[{"count":0,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/10289\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media\/13115"}],"wp:attachment":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media?parent=10289"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_cat?post=10289"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_tag?post=10289"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}