{"id":981,"date":"2018-05-21T14:06:54","date_gmt":"2018-05-21T12:06:54","guid":{"rendered":"https:\/\/ccgm.org\/produit\/globe-geologique-terrestre\/"},"modified":"2024-04-14T21:17:28","modified_gmt":"2024-04-14T19:17:28","slug":"globe-geologique-terrestre","status":"publish","type":"product","link":"https:\/\/ccgm.org\/en\/product\/globe-geological-terrestrial\/","title":{"rendered":"Geological Globe (CCGM)"},"content":{"rendered":"<p>The <strong>Geological globe<\/strong> is based on the 3rd revised edition of the <em>Geological Map of the World<\/em> at a scale of 1:25 million, published in 2014 by the <strong>Commission of the Geological Map of the World<\/strong> (CCGM). With a completely new design and cartography, the globe reflects the state of knowledge on the geology of our planet in the 21st century. This work is a synthetic compilation essentially intended for educational purposes and aims to give a better global visualization of the mega-structures and large geological ensembles that result from the events that have marked the 4 billion years of our planet's complex history.<\/p>\n<p>Geological globe<\/p>\n<p>The following is a summary of the main geological units and features:<\/p>\n<ul>\n<li>8 major stratigraphic units, from most recent to oldest: 1= Cenozoic; 2= Mesozoic; 3= Upper Paleozoic; 4= Lower Paleozoic; 5= Neoproterozoic; 6= Mesoproterozoic; 7= Paleoproterozoic; 8= Archean (&gt; 2.5 billion years old) ;<\/li>\n<li>the \"Large Magmatic Provinces\" (LIP) corresponding to large-scale magmatic pulses (continental trapps and \"oceanic shelves\"), with an indication of their average age and the extension of the \"Central Atlantic Magmatic Province\" zone has been drawn;<\/li>\n<li>the representation of the Meso-Cenozoic ophiolites, highlighting the suture zones;<\/li>\n<li>areas where the basement under the Antarctic and Greenland ice sheets is depressed below sea level;<\/li>\n<li>the continental shelf (depth &lt; 200 m) and, consequently, the continental slope;<\/li>\n<li>the continental crust\/oceanic crust (OCB) boundary;<\/li>\n<li>active subduction zones; ages and shapes of back-arc basins;<\/li>\n<li>the thrust fronts of the great orogens;<\/li>\n<li>the axes of the oceanic expansion ridges (active and fossil) marking the boundary between two divergent lithospheric plates;<\/li>\n<li>subduction zones representing the convergence of two plates and the fronts of large prisms of sedimentary accretion;<\/li>\n<li>transform faults which are a type of plate boundary between the axes of ridges and subduction zones; oceanic fracture zones, the 'scars' of transform faults;<\/li>\n<li>zones of deformation of the oceanic crust (diffuse boundary) between certain lithospheric plates;<\/li>\n<li>abnormal\" oceanic morphostructures (seamounts, \"asismic\" ripples, oceanic plateaus, traces of \"hot spots\", etc.);<\/li>\n<li>the location of submarine volcanic sequences linked to the opening of the North and South Atlantic Oceans (SDRs = Seaward Dipping Reflectors);<\/li>\n<li>45 \"hot spots\", subdivided into 4 categories; the mapping of the traces of 6 hot spots, with indication of the age of a certain number of milestones allowing to visualize the progression of the plate<\/li>\n<\/ul>\n<p>The<strong> Geological globe<\/strong> is a unique and first-class educational tool that allows a quick visualization of the major plates and subplates of global tectonics.<\/p>\n<p>Geological globe<\/p>\n<p><strong>Authors<\/strong><\/p>\n<p><strong>Philippe Bouysse<\/strong>retired marine geologist from the Bureau des Recherches G\u00e9ologiques et Mini\u00e8res (BRGM) and former Secretary General of the Commission for the Geological Map of the World (1990-2000), currently Scientific Advisor to the CCMG. Conception, synthesis and drawing of the original map.<\/p>\n<p><strong>Bruno Vrielynck<\/strong>The geologist and palaeographer of the Institut des Sciences de la Terre de Paris (Istep), Sorbonnes Universit\u00e9s\/UMPC, carried out in 2017 the complete restructuring and improvement of the GIS geo-database of the Geological Map of the World at 1:35 M.<\/p>\n<p><strong>Alain Rabaute<\/strong> (<a href=\"mailto:alain.rabaute@geosubsight.com\" target=\"_blank\" rel=\"noreferrer noopener\">GeoSubsight<\/a>), geologist and GIS expert at the Institut des Sciences de la Terre de Paris (Istep), Sorbonnes Universit\u00e9s\/UMPC, has carried out the cartographic and graphic adaptation of the Geological Map of the World geo-database for the production of the Geological Globe of the Earth.<\/p>\n<p>The manufacture of the globe was entrusted to the company <strong><em>Replogle Globes Partners LLC<\/em><\/strong> (Illinois, USA), world leader in the publishing and production of globes.<\/p>\n<p>Geological globe<\/p>","protected":false},"excerpt":{"rendered":"<p>Geological globe<\/p>\n<p>30 cm\/12\" diameter<br \/>\nScale approx. 1:42 000 000<br \/>\nPlastic globe, printed on thermoformed vinyl paper (2 hemispheres to assemble)<br \/>\nFree standing on transparent acrylic base (included)<br \/>\nManufactured for the GMPCC by Replogle<br \/>\nCCGM-CGMW 2018, Paris, France<\/p>\n<p><a href=\"https:\/\/ccgm.org\/wp-content\/uploads\/2018\/05\/cms_Legend-Earth-Geological-Globe.pdf\" target=\"_blank\" rel=\"noreferrer noopener\"><strong>Bilingual caption here<\/strong><\/a><\/p>\n<p><a href=\"https:\/\/ccgm.org\/wp-content\/uploads\/2023\/03\/Notice-Earth-Geological-Globe_2018.pdf\" target=\"_blank\" rel=\"noreferrer noopener\"><strong>Explanatory notes here<\/strong><\/a><\/p>\n<p><a href=\"https:\/\/www.geoscience.com.tw\/hardware\/ccgm\" target=\"_blank\" rel=\"noreferrer noopener\"><strong>Reseller in Taiwan here<\/strong><\/a><\/p>\n<p><strong><span style=\"color: #ff0000;\">To order the globe+maps, please place a specific order for the globe.<\/span><\/strong><\/p>","protected":false},"featured_media":971,"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 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