{"id":641,"date":"2013-06-23T21:18:20","date_gmt":"2013-06-23T19:18:20","guid":{"rendered":"https:\/\/ccgm.org\/produit\/carte-structurale-de-l-eurasie-de-l-est\/"},"modified":"2024-09-06T14:29:20","modified_gmt":"2024-09-06T12:29:20","slug":"carte-structurale-de-leurasie-orientalecarte-structurale-de-leurasie-orientalecarte-structurale-de-leurasie-orientale","status":"publish","type":"product","link":"https:\/\/ccgm.org\/es\/producto\/mapa-estructural-de-eurasia-oriental-2\/","title":{"rendered":"Mapa estructural de Eurasia Oriental"},"content":{"rendered":"<p><strong>Mapa estructural de Eurasia Oriental<\/strong><\/p>\n<p>Evoluci\u00f3n de los bloques de la corteza y los cinturones orog\u00e9nicos a lo largo del tiempo<\/p>\n<p>El mapa difiere de los mapas geol\u00f3gicos, tect\u00f3nicos y de terranas, y hace hincapi\u00e9 en la correlaci\u00f3n de los grandes cinturones euroasi\u00e1ticos. Por tanto, las unidades que se muestran no son terranos tectonoestratigr\u00e1ficos, sino una individualizaci\u00f3n de bloques estables y prismas sedimentarios y orog\u00e9nicos.<\/p>\n<p>El mapa est\u00e1 dise\u00f1ado para ofrecer una visi\u00f3n general de los cinturones tect\u00f3nicos que han contribuido al crecimiento continental del este de Eurasia.<\/p>\n<p>Los bloques y zonas estables representan unidades de corteza continental que se han comportado como entidades r\u00edgidas durante los grandes or\u00f3genos y forman la parte aut\u00f3ctona de prismas sedimentarios u orog\u00e9nicos. Estas unidades est\u00e1n separadas por cinturones orog\u00e9nicos en el mapa, pero no representan una edad espec\u00edfica.<\/p>\n<p>Por tanto, est\u00e1n representados los n\u00facleos de los principales cratones formados durante el Prec\u00e1mbrico, as\u00ed como los bloques de corteza o mesetas oce\u00e1nicas formados m\u00e1s recientemente y responsables del acortamiento de los prismas.<\/p>\n<p>Los prismas y or\u00f3genos incluyen prismas de acreci\u00f3n desarrollados mar adentro en zonas de subducci\u00f3n, pero tambi\u00e9n mar adentro en cinturones orog\u00e9nicos. Representan productos de la subducci\u00f3n, independientemente de la naturaleza -oce\u00e1nica o continental- de las costras implicadas. En su mayor\u00eda representan cinturones deformados de sedimentos, metamorfoseados o no, que actualmente se superponen a costras continentales.<\/p>\n<p><strong>Mapa estructural de Eurasia Oriental<\/strong><\/p>\n<p>Los prismas orog\u00e9nicos tambi\u00e9n pueden implicar franjas de corteza continental. En zonas complejas, sobre todo a principios del Fanerozoico, los cinturones orog\u00e9nicos est\u00e1n fuertemente metamorfoseados y pueden considerarse \"cratonizados\".<\/p>\n<p>Las Fallas se han recopilado, generalizado y clasificado por edades siempre que ha sido posible. Hab\u00eda que elegir cuando faltaba informaci\u00f3n, no estaba clara o era contradictoria. Muchas fallas tambi\u00e9n se han reactivado; el color indica la edad del evento dominante.<\/p>\n<p>Las suturas tambi\u00e9n se han clasificado cronol\u00f3gicamente, pero la edad puede variar significativamente a lo largo de ellas como consecuencia de la migraci\u00f3n del acoplamiento. En los cinturones antiguos, por erosi\u00f3n, representan el l\u00edmite de costras yuxtapuestas o superpuestas. Su alineaci\u00f3n es aproximada y puede atravesar varias alineaciones de macizos ofiol\u00edticos, lo que pone de manifiesto su posici\u00f3n al\u00f3ctona o la existencia de cierres de sistemas arco\/retroarco.<\/p>\n<p>Las facies metam\u00f3rficas se indican con puntos de color -que indican la facies dominante- para no cargar y oscurecer la informaci\u00f3n estructural.<\/p>\n<p><strong>Mapa estructural de Eurasia Oriental<\/strong><\/p>","protected":false},"excerpt":{"rendered":"<p><strong>Mapa estructural de Eurasia Oriental<\/strong><\/p>\n<p>Escala ecuatorial: 1\/12 500 000<br \/>\nPublicado en agosto de 2008<br \/>\n1 hoja :118 x 84 cm<br \/>\nCCGM-CGMW<br \/>\nAutor principal : Manuel Pubellier (CNRS-Escuela Normal Superior de Par\u00eds)<br \/>\nPrincipales colaboradores: N. Chamot-Rooke (CNRS-Ens, F. Ego (Ens), J.C. Gu\u00e9zou (CNRS), E. Konstantinovskaya (INRS-ETE), A. Rabaute (Ens-GeosubSight), J.C. Ringenbach (TOTAL)<\/p>","protected":false},"featured_media":640,"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":[59,54,62,68,69,61],"product_tag":[363,364,361,362,360],"class_list":{"0":"post-641","1":"product","2":"type-product","3":"status-publish","4":"has-post-thumbnail","6":"product_cat-tous-nos-produits","7":"product_cat-cartes","8":"product_cat-continents","9":"product_cat-europe","10":"product_cat-asie","11":"product_cat-meilleures-ventes","12":"product_tag-blocs-crustaux-eurasie","13":"product_tag-ceintures-orogeniques-eurasie","14":"product_tag-ceintures-tectoniques","15":"product_tag-croissance-continentale-de-leur","16":"product_tag-structure-geodynamique-eurasie","17":"pa_echelle-295","18":"pa_emballage-tubeexcarteroulee","19":"pa_emballage-enveloppeexcarteplieeoulivret","20":"pa_largeur-118cm","21":"pa_longueur-84cm","22":"pa_poids-0140kg","23":"desktop-align-left","24":"tablet-align-left","25":"mobile-align-left","26":"ast-product-gallery-layout-horizontal-slider","27":"ast-product-gallery-with-no-image","28":"ast-product-tabs-layout-distributed","30":"first","31":"instock","32":"shipping-taxable","33":"purchasable","34":"product-type-simple"},"_links":{"self":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/641"}],"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=641"}],"version-history":[{"count":0,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/641\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media\/640"}],"wp:attachment":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media?parent=641"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_cat?post=641"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_tag?post=641"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}