{"id":2946,"date":"2015-03-12T10:26:58","date_gmt":"2015-03-12T08:26:58","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=2946"},"modified":"2015-04-09T13:09:26","modified_gmt":"2015-04-09T11:09:26","slug":"2010-4-64-68","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2010-4-64-68\/","title":{"rendered":"2010; 4 : 64-68"},"content":{"rendered":"<p>Geoinformatika 2010; 4 : 64-68<\/p>\n<h4>POSSIBLE VARIANTS OF THE MARGINAL SEAS CLOSING IN EVOLUTION OF NEW-GUINEA-TYPE OROGENS<\/h4>\n<h5><em>Goryainov S.V.\u00a0<\/em><\/h5>\n<p style=\"text-align: justify;\">The analysis of space snapshots of New Guinea folded belt structure showed that some groups of modern volcanoes are located in the area of abnormal structure. To explain this anomaly the theoretical model of all possible variants of marginal sea closing is constructed. Some new structural variants of the process development were revealed. These variants do not taken into account by the standard models, but they are realised in discussed region. That makes it possible to construct lateral and temporary orders of elementary tectonic conditions of the marginal seas closing for the analysis of a New-Guinea-type folded belts evolution.<\/p>\n<p><strong>Keywords: <\/strong>New Guinea, plate tectonics, island arcs, marginal seas, New-Guinea-type orogen.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/07_Gorajnov.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-790 alignleft\" src=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg\" alt=\"pdf\" width=\"48\" height=\"48\" srcset=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg 128w, http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf-150x150.jpg 150w\" sizes=\"auto, (max-width: 48px) 100vw, 48px\" \/><\/a><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2010; 4 : 64-68 POSSIBLE VARIANTS OF THE MARGINAL SEAS CLOSING IN EVOLUTION OF NEW-GUINEA-TYPE OROGENS Goryainov S.V.\u00a0 The analysis of space snapshots of New Guinea folded belt structure showed that some groups of modern volcanoes are located in the area of abnormal structure. To explain this anomaly the theoretical model of all possible variants of marginal sea closing is constructed. Some new structural variants of the process development were revealed. These variants do not taken into account by the standard models, but they are realised in discussed region. That makes it possible to construct lateral and temporary orders of elementary tectonic conditions of the marginal seas closing for the analysis of a New-Guinea-type folded belts evolution. Keywords: New Guinea, plate tectonics, island arcs, marginal seas, New-Guinea-type orogen.<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"open","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-2946","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.6 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>2010; 4 : 64-68 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"http:\/\/www.geology.com.ua\/en\/2010-4-64-68\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2010; 4 : 64-68 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\" \/>\n<meta property=\"og:description\" content=\"Geoinformatika 2010; 4 : 64-68 POSSIBLE VARIANTS OF THE MARGINAL SEAS CLOSING IN EVOLUTION OF NEW-GUINEA-TYPE OROGENS Goryainov S.V.\u00a0 The analysis of space snapshots of New Guinea folded belt structure showed that some groups of modern volcanoes are located in the area of abnormal structure. To explain this anomaly the theoretical model of all possible variants of marginal sea closing is constructed. Some new structural variants of the process development were revealed. These variants do not taken into account by the standard models, but they are realised in discussed region. That makes it possible to construct lateral and temporary orders of elementary tectonic conditions of the marginal seas closing for the analysis of a New-Guinea-type folded belts evolution. Keywords: New Guinea, plate tectonics, island arcs, marginal seas, New-Guinea-type orogen.\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2010-4-64-68\/\" \/>\n<meta property=\"og:site_name\" content=\"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\" \/>\n<meta property=\"article:modified_time\" content=\"2015-04-09T11:09:26+00:00\" \/>\n<meta property=\"og:image\" content=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"1 minute\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2010-4-64-68\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2010-4-64-68\\\/\",\"name\":\"2010; 4 : 64-68 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\",\"isPartOf\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2010-4-64-68\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2010-4-64-68\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-03-12T08:26:58+00:00\",\"dateModified\":\"2015-04-09T11:09:26+00:00\",\"breadcrumb\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2010-4-64-68\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2010-4-64-68\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2010-4-64-68\\\/#primaryimage\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"contentUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2010-4-64-68\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"2010; 4 : 64-68\"}]},{\"@type\":\"WebSite\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\",\"name\":\"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\",\"description\":\"\u0426\u0435\u043d\u0442\u0440 \u043c\u0435\u043d\u0435\u0434\u0436\u043c\u0435\u043d\u0442\u0443 \u0442\u0430 \u043c\u0430\u0440\u043a\u0435\u0442\u0438\u043d\u0433\u0443 \u0432 \u0433\u0430\u043b\u0443\u0437\u0456 \u043d\u0430\u0443\u043a \u043f\u0440\u043e \u0417\u0435\u043c\u043b\u044e\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"2010; 4 : 64-68 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"http:\/\/www.geology.com.ua\/en\/2010-4-64-68\/","og_locale":"en_US","og_type":"article","og_title":"2010; 4 : 64-68 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","og_description":"Geoinformatika 2010; 4 : 64-68 POSSIBLE VARIANTS OF THE MARGINAL SEAS CLOSING IN EVOLUTION OF NEW-GUINEA-TYPE OROGENS Goryainov S.V.\u00a0 The analysis of space snapshots of New Guinea folded belt structure showed that some groups of modern volcanoes are located in the area of abnormal structure. To explain this anomaly the theoretical model of all possible variants of marginal sea closing is constructed. Some new structural variants of the process development were revealed. These variants do not taken into account by the standard models, but they are realised in discussed region. That makes it possible to construct lateral and temporary orders of elementary tectonic conditions of the marginal seas closing for the analysis of a New-Guinea-type folded belts evolution. 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