{"id":710,"date":"2013-06-23T23:04:56","date_gmt":"2013-06-23T21:04:56","guid":{"rendered":"https:\/\/ccgm.org\/produit\/carte-geologique-des-regions-oceaniques-et-continentales-d-europe-du-nord\/"},"modified":"2025-02-22T22:24:07","modified_gmt":"2025-02-22T21:24:07","slug":"carte-geologique-des-regions-oceaniques-et-continentales-deurope-du-nord","status":"publish","type":"product","link":"https:\/\/ccgm.org\/es\/producto\/mapa-geologico-de-las-regiones-oceanicas-y-continentales-del-norte-de-europa-2\/","title":{"rendered":"Mapa geol\u00f3gico de las regiones oce\u00e1nicas y continentales del norte de Europa"},"content":{"rendered":"<p><strong>Mapa geol\u00f3gico de las regiones oce\u00e1nicas y continentales del norte de Europa<\/strong><\/p>\n<p>El Servicio Geol\u00f3gico Noruego (NGU), en colaboraci\u00f3n con los servicios geol\u00f3gicos de 22 pa\u00edses europeos, ha cartografiado el basamento precuaternario del norte de Europa a escala 1:4 millones.<\/p>\n<p>Por primera vez hasta 2002, se presenta la geolog\u00eda de las formaciones continentales y oce\u00e1nicas de las regiones en su conjunto. La zona abarcada se extiende longitudinalmente desde el este de Groenlandia hasta Nueva Zelanda y latitudinalmente desde Svalbard hasta el noreste de la costa francesa; tambi\u00e9n se incluye la parte occidental de la plataforma rusa.<\/p>\n<p>La geolog\u00eda incluye rocas de todas las edades, desde gneises del Arcaico hasta basaltos recientes de la dorsal mesoatl\u00e1ntica, excepto sedimentos cuaternarios. Adem\u00e1s de la geolog\u00eda del basamento, se han representado zonas de falla, escarpes, ejes de acreci\u00f3n, anomal\u00edas magn\u00e9ticas y l\u00edmites de la corteza continental-oce\u00e1nica. Se incluyeron catorce secciones transversales, as\u00ed como perfiles de perforaciones profundas en las zonas oce\u00e1nicas.<\/p>\n<p>Los pa\u00edses que participaron en su realizaci\u00f3n son :<br \/>\nAlemania, B\u00e9lgica, Dinamarca, Eslovaquia, Estonia, Finlandia, Francia, Irlanda, Islandia, Letonia, Lituania, Luxemburgo, Noruega, Pa\u00edses Bajos, Polonia, Reino Unido, Rep\u00fablica Checa, Rusia, Suecia y Ucrania.<\/p>\n<p>Este proyecto cartogr\u00e1fico cont\u00f3 con el apoyo financiero del Servicio Geol\u00f3gico Noruego y de las siguientes empresas petroleras: Amerada Hess Norge A\/S, Mobil Exploration Norway Inc, Norsk Agip A\/S, Norsk Hydro ASA, Phillips Petroleum Company Norway, Saga Petroleum a.s. (ahora Norsk Hydro ASA) y Statoil ASA.<\/p>\n<p>La edici\u00f3n impresa del mapa se ha publicado en dos idiomas, noruego e ingl\u00e9s. Tambi\u00e9n hay una versi\u00f3n digital disponible en el sitio web del Servicio Geol\u00f3gico Noruego: <a href=\"http:\/\/www.ngu.no\" target=\"_blank\" rel=\"noreferrer noopener\">www.ngu.no<\/a>.<\/p>\n<p><strong>Mapa geol\u00f3gico de las regiones oce\u00e1nicas y continentales del norte de Europa<\/strong><\/p>","protected":false},"excerpt":{"rendered":"<p><strong>Mapa geol\u00f3gico de las regiones oce\u00e1nicas y continentales del norte de Europa<\/strong><\/p>\n<p>Escala: 1:4 000 000<br \/>\nPublicado en 2002 por el Servicio Geol\u00f3gico de Noruega<br \/>\nTama\u00f1o de 1 hoja: 140 cm x 100 cm<br \/>\nEn ingl\u00e9s y noruego. Notas explicativas en ingl\u00e9s.<\/p>\n<p>Coordinador principal :<br \/>\nDra. Ellen M.O. Sigmond (NGU)<br \/>\nNGU, 2002<\/p>\n<p><strong>Mapa geol\u00f3gico de las regiones oce\u00e1nicas y continentales del norte de Europa<\/strong><\/p>","protected":false},"featured_media":709,"comment_status":"closed","ping_status":"closed","template":"","meta":{"inline_featured_image":false,"site-sidebar-layout":"default","site-content-layout":"default","ast-site-content-layout":"","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":"default","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":[59,54,62,68,64],"product_tag":[424,423,425],"class_list":{"0":"post-710","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-oceans","11":"product_tag-formations-continentales-et-ocea","12":"product_tag-geologie-nw-europe","13":"product_tag-socles-pre-quaternaires-du-nord","14":"pa_echelle-286","15":"pa_emballage-tubeexcarteroulee","16":"pa_emballage-enveloppeexcarteplieeoulivret","17":"pa_largeur-100cm","18":"pa_longueur-140cm","19":"pa_poids-0160kg","20":"desktop-align-left","21":"tablet-align-left","22":"mobile-align-left","23":"ast-product-gallery-layout-horizontal-slider","24":"ast-product-gallery-with-no-image","25":"ast-product-tabs-layout-distributed","27":"first","28":"instock","29":"shipping-taxable","30":"purchasable","31":"product-type-simple"},"_links":{"self":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/710"}],"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=710"}],"version-history":[{"count":0,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/710\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media\/709"}],"wp:attachment":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media?parent=710"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_cat?post=710"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_tag?post=710"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}