{"id":954,"date":"2017-02-18T15:39:49","date_gmt":"2017-02-18T14:39:49","guid":{"rendered":"https:\/\/ccgm.org\/produit\/carte-structurale-de-la-mer-de-chine-du-sud\/"},"modified":"2024-09-06T14:31:03","modified_gmt":"2024-09-06T12:31:03","slug":"carte-structurale-de-la-mer-de-chine-du-sud","status":"publish","type":"product","link":"https:\/\/ccgm.org\/es\/producto\/mapa-estructural-del-mar-sur-2\/","title":{"rendered":"Mapa estructural del Mar de China Meridional"},"content":{"rendered":"<p><strong>Mapa estructural del Mar de China Meridional<\/strong><\/p>\n<p>Este mapa estructural del Mar de China Meridional sintetiza un gran volumen de datos procedentes de la investigaci\u00f3n acad\u00e9mica e industrial. Su objetivo es presentar las principales estructuras que han desempe\u00f1ado un papel clave en la formaci\u00f3n y evoluci\u00f3n del Mar de China Meridional.<\/p>\n<p>Los colores de los rasgos representados en el mapa se han elegido para facilitar la correlaci\u00f3n de las partes continental y oce\u00e1nica de las unidades estructurales. No se han diferenciado las rocas del basamento antejur\u00e1sico, pero se ha prestado especial atenci\u00f3n a los granitoides mesozoicos, las rocas magm\u00e1ticas y metam\u00f3rficas y los edificios volc\u00e1nicos cenozoicos situados mar adentro y en el fondo marino.<\/p>\n<p><strong>Mapa estructural del Mar de China Meridional<\/strong><\/p>\n<p>Los principales dominios de la corteza que se distinguen son: el basamento continental grueso, la corteza continental estirada, las zonas del manto supuestamente exhumadas (incluso bajo los sedimentos post-acrecionarios), la corteza de arco volc\u00e1nico en Filipinas y la corteza oce\u00e1nica. En los dominios continental y oce\u00e1nico est\u00e1n representados: los sedimentos de prismas, plataformas y cuencas, as\u00ed como la extensi\u00f3n de los ambientes marinos mesozoicos.<\/p>\n<p>No se ha especificado la edad de la corteza en las cuencas distintas de las del Mar de China Meridional (Mar de C\u00e9lebes, Mar de Sul\u00fa). Las cuencas cenozoicas distendidas est\u00e1n resaltadas y se muestran en transparencia por encima de las estructuras de acreci\u00f3n.  En lugar de mostrar picos o patrones de anomal\u00edas magn\u00e9ticas que a\u00fan est\u00e1n abiertos a discusi\u00f3n, el mapa muestra anomal\u00edas magn\u00e9ticas incontroladas, destacando as\u00ed el marco estructural del fondo oce\u00e1nico.<\/p>\n<p>Las fallas que aparecen en el mapa son las asociadas a la extensi\u00f3n de la corteza durante el Cret\u00e1cico temprano.  Otras fallas, inversas o de cabalgamiento, creadas durante el Mioceno Medio y el Plioceno, pueden ser oblicuas o paralelas a las fallas de acreci\u00f3n. La representaci\u00f3n, en finas l\u00edneas rojas, destaca las fallas superficiales que caracterizan la tect\u00f3nica gravitatoria que afecta a los potentes deltas miocenos del Mar de China Meridional.<\/p>\n<p>El mapa se complementa con una secci\u00f3n basada en datos publicados de la literatura internacional. Esta secci\u00f3n proporciona una imagen muy bonita de un margen hiperestirado que afecta a un batolito.<\/p>\n<p>La leyenda puede descargarse haciendo clic en <a title=\"Leyenda Mapa Mar de China Meridional\" href=\"https:\/\/ccgm.org\/wp-content\/uploads\/2017\/02\/cms_Legend-Map-South-China-Sea.pdf\" target=\"_blank\" rel=\"noreferrer noopener\">aqu\u00ed<\/a><\/p>\n<p>Fondo topobatim\u00e9trico: SRTM30+ v1.0, publicado en noviembre de 2004, v\u00e9ase: http:\/\/topex.ucsd.edu\/WWW_html\/srtm30_plus<\/p>\n<p>Altimetr\u00eda a partir de las bases de datos SRTM y GEBCO.<\/p>\n<p>doi:10.14682\/2017STRUCTUSCS<\/p>\n<p><strong>Mapa estructural del Mar de China Meridional<\/strong><\/p>","protected":false},"excerpt":{"rendered":"<p><strong>Mapa estructural del Mar de China Meridional<\/strong><\/p>\n<p>1\u00aa edici\u00f3n, escala 1:3 000 000<br \/>\nProyecci\u00f3n: Equidistante de Mercator<br \/>\nDimensiones: 118,5 x 84 cm<br \/>\nAutores: M. Pubellier, D. Savva, M. Aurelio, F. Sapin<br \/>\nColaboradores: J.L Auxi\u00e8tre, N. Chamot-Rooke, L.S. Chan, H. Darman, M. Delescluse, D.Franke, V. Le Gal, C.S. Liu, M. Madon, Y. Mansor, K. McIntosh, D. Menier, F. Meresse, V. P. Phung, B. Sautter, J-C. Sibuet, S. Steuer, K. Taguibao, V.T. Tran<strong><br \/>\n\u00a9 <\/strong>CCGM-CGMW 2017<\/p>\n<p><strong>Mapa estructural del Mar de China Meridional<\/strong><\/p>","protected":false},"featured_media":951,"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":[59,54,62,69,64],"product_tag":[],"class_list":{"0":"post-954","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-asie","10":"product_cat-oceans","11":"pa_echelle-305","12":"pa_emballage-tubeexcarteroulee","13":"pa_emballage-enveloppeexcarteplieeoulivret","14":"pa_largeur-85cm","15":"pa_longueur-118_5cm","16":"pa_poids-0150kg","17":"desktop-align-left","18":"tablet-align-left","19":"mobile-align-left","20":"ast-product-gallery-layout-horizontal-slider","21":"ast-product-tabs-layout-distributed","23":"first","24":"instock","25":"shipping-taxable","26":"purchasable","27":"product-type-simple"},"_links":{"self":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/954"}],"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=954"}],"version-history":[{"count":0,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/954\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media\/951"}],"wp:attachment":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media?parent=954"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_cat?post=954"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_tag?post=954"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}