{"id":3257,"date":"2015-03-25T12:32:40","date_gmt":"2015-03-25T10:32:40","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=3257"},"modified":"2015-03-25T12:32:40","modified_gmt":"2015-03-25T10:32:40","slug":"2009-3-48-55","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2009-3-48-55\/","title":{"rendered":"2009; 3 : 48-55"},"content":{"rendered":"<p>Geoinformatika 2009; 3 :\u00a048-55<\/p>\n<h4>GENERAL CHARACTERISTICS OF PETROPHYSICAL PROPERTIES OF ROCKS IN THE PRE-NEOGENE BASEMENT OF THE OUTER\u00a0 CARPATHIAN FOREDEEP<\/h4>\n<h5><em>Kurovets I.M., Prytulka H.Y., Shyra A.I., Shuflyak Yu.E.<\/em><\/h5>\n<p style=\"text-align: justify;\">As a result of complex laboratory studies of core material it became possible to investigate petrophysical characteristics of rocks in the Pre-Neogene basement, their lithological-facial and structural-textural features and to establish the main geological factors determining their capacity-filtration properties. Methods of mathematical statistics were used to analyse petrophysical parameters of rock samples from the Mesozoic and Paleozoic deposits.\u00a0 The greatest range of the change in the porosity factor is characteristic of sandstones and aleurolites of the Cretaceous (0,1\u201328,8 %) and the Upper Jurassic (0,4\u201324,6 %), and the least one is characteristic of terrigenous rocks of the Paleozoic that underwent the greatest influence of katagenic processes. The intergranular porosity of carbonate rocks becomes changed within the limits of 0,1\u201317,3 %. A regular decrease in porosity and permeability of terrigenous rocks with depth is typical. For carbonate rocks the change in capacity-filtration parameters with depth is less noticeable.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/Kurovets.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; 3 :\u00a048-55 GENERAL CHARACTERISTICS OF PETROPHYSICAL PROPERTIES OF ROCKS IN THE PRE-NEOGENE BASEMENT OF THE OUTER\u00a0 CARPATHIAN FOREDEEP Kurovets I.M., Prytulka H.Y., Shyra A.I., Shuflyak Yu.E. As a result of complex laboratory studies of core material it became possible to investigate petrophysical characteristics of rocks in the Pre-Neogene basement, their lithological-facial and structural-textural features and to establish the main geological factors determining their capacity-filtration properties. Methods of mathematical statistics were used to analyse petrophysical parameters of rock samples from the Mesozoic and Paleozoic deposits.\u00a0 The greatest range of the change in the porosity factor is characteristic of sandstones and aleurolites of the Cretaceous (0,1\u201328,8 %) and the Upper Jurassic (0,4\u201324,6 %), and the least one is characteristic of terrigenous rocks of the Paleozoic that underwent the greatest influence of katagenic processes. The intergranular porosity of carbonate rocks becomes changed within the limits of 0,1\u201317,3 %. A regular decrease in porosity and permeability of terrigenous rocks with depth is typical. For carbonate rocks the change in capacity-filtration parameters with depth is less noticeable.<\/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-3257","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; 3 : 48-55 - \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\/2009-3-48-55\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2009; 3 : 48-55 - \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; 3 :\u00a048-55 GENERAL CHARACTERISTICS OF PETROPHYSICAL PROPERTIES OF ROCKS IN THE PRE-NEOGENE BASEMENT OF THE OUTER\u00a0 CARPATHIAN FOREDEEP Kurovets I.M., Prytulka H.Y., Shyra A.I., Shuflyak Yu.E. As a result of complex laboratory studies of core material it became possible to investigate petrophysical characteristics of rocks in the Pre-Neogene basement, their lithological-facial and structural-textural features and to establish the main geological factors determining their capacity-filtration properties. Methods of mathematical statistics were used to analyse petrophysical parameters of rock samples from the Mesozoic and Paleozoic deposits.\u00a0 The greatest range of the change in the porosity factor is characteristic of sandstones and aleurolites of the Cretaceous (0,1\u201328,8 %) and the Upper Jurassic (0,4\u201324,6 %), and the least one is characteristic of terrigenous rocks of the Paleozoic that underwent the greatest influence of katagenic processes. The intergranular porosity of carbonate rocks becomes changed within the limits of 0,1\u201317,3 %. A regular decrease in porosity and permeability of terrigenous rocks with depth is typical. For carbonate rocks the change in capacity-filtration parameters with depth is less noticeable.\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2009-3-48-55\/\" \/>\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=\"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\\\/2009-3-48-55\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-48-55\\\/\",\"name\":\"2009; 3 : 48-55 - \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\\\/2009-3-48-55\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-48-55\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-03-25T10:32:40+00:00\",\"breadcrumb\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-48-55\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-48-55\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-48-55\\\/#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\\\/2009-3-48-55\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"2009; 3 : 48-55\"}]},{\"@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; 3 : 48-55 - \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\/2009-3-48-55\/","og_locale":"en_US","og_type":"article","og_title":"2009; 3 : 48-55 - \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; 3 :\u00a048-55 GENERAL CHARACTERISTICS OF PETROPHYSICAL PROPERTIES OF ROCKS IN THE PRE-NEOGENE BASEMENT OF THE OUTER\u00a0 CARPATHIAN FOREDEEP Kurovets I.M., Prytulka H.Y., Shyra A.I., Shuflyak Yu.E. As a result of complex laboratory studies of core material it became possible to investigate petrophysical characteristics of rocks in the Pre-Neogene basement, their lithological-facial and structural-textural features and to establish the main geological factors determining their capacity-filtration properties. Methods of mathematical statistics were used to analyse petrophysical parameters of rock samples from the Mesozoic and Paleozoic deposits.\u00a0 The greatest range of the change in the porosity factor is characteristic of sandstones and aleurolites of the Cretaceous (0,1\u201328,8 %) and the Upper Jurassic (0,4\u201324,6 %), and the least one is characteristic of terrigenous rocks of the Paleozoic that underwent the greatest influence of katagenic processes. The intergranular porosity of carbonate rocks becomes changed within the limits of 0,1\u201317,3 %. A regular decrease in porosity and permeability of terrigenous rocks with depth is typical. 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