{"id":3224,"date":"2015-03-24T15:12:05","date_gmt":"2015-03-24T13:12:05","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=3224"},"modified":"2015-04-10T11:51:20","modified_gmt":"2015-04-10T09:51:20","slug":"2009-4-87-92","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2009-4-87-92\/","title":{"rendered":"2009; 4 : 87-92"},"content":{"rendered":"<p>Geoinformatika 2009; 4 : 87-92<\/p>\n<h4>RESULT OF PALEOMAGNETIC RESEARCH OF SARMATIAN DEPOSITS PROFILE IN THE MIKHAILOVSKY QUARRY<\/h4>\n<h5><em>Slivinskaya G.V.<\/em><\/h5>\n<p style=\"text-align: justify;\">The paper reports on a magnetostratigraphic study of the middle and upper sarmatian sedimentary rocks in the section of the Mikhailovsky quarry from the south of Ukraine. The standard procedure of the samples demagnetization by an alternating magnetic field and temperature, as well as the Kirshvink analysis allowed to separate the NRM components and to determine the primary characteristic <i>J<\/i><em><sub>n<\/sub><sub>0\u00a0<\/sub><\/em>component. Based on the data, the regional magnetostratigraphic section of Mikhailovsky quarry was constructed. It marks the state of geomagnetic field in the Late Neogene time interval and contains reliable paleomagnetic benchmarks for stratifying and correlating similar masses within Eastern Paratethys.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/Slivinska1.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 2009; 4 : 87-92 RESULT OF PALEOMAGNETIC RESEARCH OF SARMATIAN DEPOSITS PROFILE IN THE MIKHAILOVSKY QUARRY Slivinskaya G.V. The paper reports on a magnetostratigraphic study of the middle and upper sarmatian sedimentary rocks in the section of the Mikhailovsky quarry from the south of Ukraine. The standard procedure of the samples demagnetization by an alternating magnetic field and temperature, as well as the Kirshvink analysis allowed to separate the NRM components and to determine the primary characteristic Jn0\u00a0component. Based on the data, the regional magnetostratigraphic section of Mikhailovsky quarry was constructed. It marks the state of geomagnetic field in the Late Neogene time interval and contains reliable paleomagnetic benchmarks for stratifying and correlating similar masses within Eastern Paratethys.<\/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-3224","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>2009; 4 : 87-92 - \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\/2009-4-87-92\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2009; 4 : 87-92 - \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 2009; 4 : 87-92 RESULT OF PALEOMAGNETIC RESEARCH OF SARMATIAN DEPOSITS PROFILE IN THE MIKHAILOVSKY QUARRY Slivinskaya G.V. The paper reports on a magnetostratigraphic study of the middle and upper sarmatian sedimentary rocks in the section of the Mikhailovsky quarry from the south of Ukraine. The standard procedure of the samples demagnetization by an alternating magnetic field and temperature, as well as the Kirshvink analysis allowed to separate the NRM components and to determine the primary characteristic Jn0\u00a0component. Based on the data, the regional magnetostratigraphic section of Mikhailovsky quarry was constructed. It marks the state of geomagnetic field in the Late Neogene time interval and contains reliable paleomagnetic benchmarks for stratifying and correlating similar masses within Eastern Paratethys.\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2009-4-87-92\/\" \/>\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=\"2015-04-10T09:51:20+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\\\/2009-4-87-92\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-4-87-92\\\/\",\"name\":\"2009; 4 : 87-92 - \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\\\/2009-4-87-92\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-4-87-92\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-03-24T13:12:05+00:00\",\"dateModified\":\"2015-04-10T09:51:20+00:00\",\"breadcrumb\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-4-87-92\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-4-87-92\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-4-87-92\\\/#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\\\/2009-4-87-92\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"2009; 4 : 87-92\"}]},{\"@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":"2009; 4 : 87-92 - \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\/2009-4-87-92\/","og_locale":"en_US","og_type":"article","og_title":"2009; 4 : 87-92 - \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 2009; 4 : 87-92 RESULT OF PALEOMAGNETIC RESEARCH OF SARMATIAN DEPOSITS PROFILE IN THE MIKHAILOVSKY QUARRY Slivinskaya G.V. The paper reports on a magnetostratigraphic study of the middle and upper sarmatian sedimentary rocks in the section of the Mikhailovsky quarry from the south of Ukraine. The standard procedure of the samples demagnetization by an alternating magnetic field and temperature, as well as the Kirshvink analysis allowed to separate the NRM components and to determine the primary characteristic Jn0\u00a0component. Based on the data, the regional magnetostratigraphic section of Mikhailovsky quarry was constructed. It marks the state of geomagnetic field in the Late Neogene time interval and contains reliable paleomagnetic benchmarks for stratifying and correlating similar masses within Eastern Paratethys.","og_url":"http:\/\/www.geology.com.ua\/en\/2009-4-87-92\/","og_site_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","article_modified_time":"2015-04-10T09:51:20+00:00","og_image":[{"url":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg","type":"","width":"","height":""}],"twitter_misc":{"Est. reading time":"1 minute"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"http:\/\/www.geology.com.ua\/en\/2009-4-87-92\/","url":"http:\/\/www.geology.com.ua\/en\/2009-4-87-92\/","name":"2009; 4 : 87-92 - \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\/2009-4-87-92\/#primaryimage"},"image":{"@id":"http:\/\/www.geology.com.ua\/en\/2009-4-87-92\/#primaryimage"},"thumbnailUrl":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg","datePublished":"2015-03-24T13:12:05+00:00","dateModified":"2015-04-10T09:51:20+00:00","breadcrumb":{"@id":"http:\/\/www.geology.com.ua\/en\/2009-4-87-92\/#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":[["http:\/\/www.geology.com.ua\/en\/2009-4-87-92\/"]]}]},{"@type":"ImageObject","inLanguage":"en-US","@id":"http:\/\/www.geology.com.ua\/en\/2009-4-87-92\/#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\/2009-4-87-92\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"http:\/\/www.geology.com.ua\/en\/"},{"@type":"ListItem","position":2,"name":"2009; 4 : 87-92"}]},{"@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"}]}},"_links":{"self":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/3224","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/comments?post=3224"}],"version-history":[{"count":2,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/3224\/revisions"}],"predecessor-version":[{"id":3790,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/3224\/revisions\/3790"}],"wp:attachment":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/media?parent=3224"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}