{"id":1250,"date":"2022-07-04T11:40:18","date_gmt":"2022-07-04T09:40:18","guid":{"rendered":"https:\/\/ccgm.org\/?post_type=product&#038;p=1250"},"modified":"2024-10-25T18:14:09","modified_gmt":"2024-10-25T16:14:09","slug":"atlas-peri-tethys-des-cartes-paleogeographiques-pdf","status":"publish","type":"product","link":"https:\/\/ccgm.org\/es\/producto\/atlas-peri-tethys-de-mapas-paleogeograficos-pdf\/","title":{"rendered":"Atlas Peri-Tethys de Mapas Paleogeogr\u00e1ficos-PDF"},"content":{"rendered":"<p><strong>Atlas Peri-Tethys de Mapas Paleogeogr\u00e1ficos-PDF<\/strong><\/p>\n<p><strong>Nota: Este atlas est\u00e1 sujeto a un acuerdo de licencia.<\/strong><\/p>\n<p>El Atlas Peri-Tethys de Mapas Paleogeogr\u00e1ficos es el resultado de un programa internacional que feder\u00f3 entre 1994 y 1999 los esfuerzos de 13 instituciones acad\u00e9micas y de varias empresas p\u00fablicas y petroleras (BRGM, Elf, IFP, Agip, Arco, Chevron, Conoco, Exxon, Shell, Sonatrach Total), bajo la coordinaci\u00f3n general de la Universidad Pierre et Marie Curie. El Atlas presenta reconstrucciones paleogeogr\u00e1ficas de los m\u00e1rgenes del Tethys que abarcan el periodo comprendido entre el Muscoviano (Paleozoico Superior) y el \u00daltimo M\u00e1ximo Glacial. M\u00e1s de 250 cient\u00edficos de 30 pa\u00edses han contribuido al Atlas. La totalidad de las publicaciones resultantes de este programa incluye art\u00edculos de m\u00e1s de 1000 autores.<\/p>\n<p><strong>Contenido del Atlas<\/strong><\/p>\n<p>El juego incluye 24 mapas a escala 1:10.000.000 de cada uno de los periodos que se indican a continuaci\u00f3n y un volumen de notas explicativas en ingl\u00e9s.<\/p>\n<table style=\"width: 610px; height: 150px;\" border=\"0\" cellspacing=\"0\" cellpadding=\"0\">\n<tbody>\n<tr>\n<td valign=\"top\" width=\"213\">\n<ul>\n<li>Moscovita<\/li>\n<li>Artinskien<\/li>\n<li>Wordien<\/li>\n<li>Oleaner<\/li>\n<li>Ladino temprano<\/li>\n<li>Noriana superior<\/li>\n<li>Sinemuriano superior<\/li>\n<li>Toarciano medio<\/li>\n<\/ul>\n<\/td>\n<td valign=\"top\" width=\"217\">\n<ul>\n<li>Calloviano medio<\/li>\n<li>Kimmeridgiense inferior<\/li>\n<li>Tithoniano inferior<\/li>\n<li>Hauterivien<\/li>\n<li>Aptiano inferior<\/li>\n<li>Cenomaniense superior<\/li>\n<li>Campaniense<\/li>\n<li>Maastrichtiano superior<\/li>\n<\/ul>\n<\/td>\n<td valign=\"top\" width=\"217\">\n<ul>\n<li>Ypresiano medio<\/li>\n<li>Luteciano superior<\/li>\n<li>Rupeliano superior<\/li>\n<li>Burdigaliano inferior<\/li>\n<li>Bajo Langhien<\/li>\n<li>Tortoniense superior<\/li>\n<li>Piacenzian<\/li>\n<li>\u00daltimo M\u00e1ximo Glacial<\/li>\n<\/ul>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p>Los elementos de la leyenda incluyen :<\/p>\n<ul>\n<li>16 medios sedimentarios<\/li>\n<li>21 tipos de roca<\/li>\n<li>Paleograf\u00eda del litoral, corrientes marinas o patrones de flujo hidrosedimentario<\/li>\n<li>Balance h\u00eddrico (por ejemplo, convecci\u00f3n termohalina con estancamiento profundo en cuencas aisladas)<\/li>\n<li>Tendencias en las transferencias regionales de sedimentos<\/li>\n<li>Tr\u00e1fico e\u00f3lico<\/li>\n<li>S\u00edmbolos tect\u00f3nicos<\/li>\n<\/ul>\n<p>El Atlas Peri-Tethys de Mapas Paleogeogr\u00e1ficos-PDF abarca un periodo de 300 Ma e ilustra :<\/p>\n<ul>\n<li>La evoluci\u00f3n de las zonas sedimentarias en relaci\u00f3n con la extensi\u00f3n y compresi\u00f3n tect\u00f3nicas<\/li>\n<li>Dep\u00f3sitos sedimentarios de origen eust\u00e1tico<\/li>\n<li>Piscinas relacionadas con la compresi\u00f3n<\/li>\n<li>Zonas permanentemente expuestas<\/li>\n<\/ul>\n<p>Para determinar los acontecimientos ocurridos durante los cortos periodos representados en cada mapa (3 a 5 Ma), fue necesario :<\/p>\n<ul>\n<li>Establecer escalas cronoestratigr\u00e1ficas precisas, especialmente escalas paleontol\u00f3gicas;<\/li>\n<li>determinar los reg\u00edmenes de tensiones y establecer las interpretaciones pertinentes en el contexto de la tect\u00f3nica de placas, y<\/li>\n<li>realizar an\u00e1lisis geodin\u00e1micos de los procesos de llenado y deformaci\u00f3n de las cuencas principales.<\/li>\n<\/ul>\n<p>Atlas Peri-Tethys de Mapas Paleogeogr\u00e1ficos-PDF permite :<\/p>\n<ul>\n<li>El estudio de las variaciones clim\u00e1ticas asociadas a la extensi\u00f3n de los mares epicontinentales, la evoluci\u00f3n de las formas del relieve y su influencia en las facies (se han caracterizado 78, 21 de las cuales son de gran importancia);<\/li>\n<\/ul>\n<ul>\n<li>para determinar la extensi\u00f3n de los biotopos, que son esenciales para comprender su evoluci\u00f3n paleontol\u00f3gica;<\/li>\n<li>predecir el comportamiento y las caracter\u00edsticas de llenado de las cuencas sedimentarias, y<\/li>\n<li>seguir la evoluci\u00f3n tect\u00f3nica de las plataformas peri-Tethyanas.<\/li>\n<li><\/li>\n<\/ul>\n<p>Puedes descargarte la lista de publicaciones (Memorandos y correlaciones) que completan el Atlas<a title=\"Publicaciones de Peri-Tethys\" href=\"https:\/\/ccgm.org\/wp-content\/uploads\/2022\/01\/cms_Peri-Tethys-programme-publications.doc\" target=\"_blank\" rel=\"noreferrer noopener\"> aqu\u00ed<\/a>.<\/p>\n<p>Patrocinadores: AGIP, ARCO, BRGM, CHEVRON, CNRS-INSU, CONOCO, EAP (ELF), EXXON, IFP, SHELL, SONATRACH, TOTAL &amp; UPMC.<\/p>","protected":false},"excerpt":{"rendered":"<p><strong>Atlas Peri-Tethys de Mapas Paleogeogr\u00e1ficos-PDF<\/strong><\/p>\n<p>24 cartas, cada una con una leyenda<br \/>\n<strong>S\u00f3lo disponible en formato pdf.<\/strong><br \/>\nNotas explicativas en ingl\u00e9s, S. Crasquin, Coordinador<br \/>\nEditores: J. Dercourt, M. Gaetani, B. Vrielynck, E. Barrier, B. Biju-Duval, M.F. Brunet, J.P. Cadet, S. Crasquin y M. Sandulescu<br \/>\nPar\u00eds, 2000<\/p>","protected":false},"featured_media":9301,"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":[59,55,56],"product_tag":[552,556,554,555,553],"class_list":{"0":"post-1250","1":"product","2":"type-product","3":"status-publish","4":"has-post-thumbnail","6":"product_cat-tous-nos-produits","7":"product_cat-versions-numeriques-des-cartes-et-livrets","8":"product_cat-livrets","9":"product_tag-atlas-peri-tethys","10":"product_tag-cartes-paleogeographiques-de-la","11":"product_tag-paleo-environnements","12":"product_tag-paleo-tectonique-de-la-mer-tethy","13":"product_tag-programme-peri-tethys","14":"desktop-align-left","15":"tablet-align-left","16":"mobile-align-left","17":"ast-product-gallery-layout-horizontal-slider","18":"ast-product-tabs-layout-distributed","20":"first","21":"instock","22":"downloadable","23":"virtual","24":"sold-individually","25":"purchasable","26":"product-type-simple"},"_links":{"self":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/1250"}],"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=1250"}],"version-history":[{"count":0,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product\/1250\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media\/9301"}],"wp:attachment":[{"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/media?parent=1250"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_cat?post=1250"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/ccgm.org\/es\/wp-json\/wp\/v2\/product_tag?post=1250"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}