{"id":7665,"date":"2019-04-04T15:52:01","date_gmt":"2019-04-04T13:52:01","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=7665"},"modified":"2021-05-23T15:02:58","modified_gmt":"2021-05-23T13:02:58","slug":"7665-2","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/7665-2\/","title":{"rendered":""},"content":{"rendered":"<p><\/p>\n<p style=\"text-align: justify\"><em>Geoinformatika 2019; 1(69) : 58-61<\/em><\/p>\n<p style=\"text-align: justify\">\u0423\u0414\u041a 528.88 (914\/919):629.783<\/p>\n<h4 style=\"text-align: justify\"><strong>THE APPROACH TO USE OF REMOTE SENSING DATA FOR DEFINITION THE DIP AND STRIKE OF ROCK LAYERS<\/strong><\/h4>\n<h5 style=\"text-align: justify\">V.I. Zatserkovnyi\u00a0, I.V. Tishaiev, O.M. Pylypenko<\/h5>\n<p style=\"text-align: justify\"><em>Taras Shevchenko National University of Kyiv, Institute of Geology, 90, Vasylkivska Str., Kyiv, 03022, Ukraine, e-mail: zvigis@mail.ru, ivantishaev@yandex.ru, ya.ne.haker@yandex.ua <\/em><\/p>\n<p style=\"text-align: justify\"><strong>Purpose.<\/strong> It is investigated the approach to the use the remote sensing data for finding the dip and strike of rock layers. A geometric model for approximation surfaces of rock layers and finding spatial orientation elements, can be designed and deployed based on the remote sensing data.<br \/>\n<strong>Design\/methodology\/approach.<\/strong> The methodology was implemented as workflow. Geological recognition (manual or automatized) of remote sensing data (optical range) consists of identification lithological types and tracing edge polylines between neighbors types. Automated extraction spatial information from Digital Elevation Model (DEM) for each vertex of edge polylines. Calculation spatial orientation elements of surfaces for each conjunction of\u00a0 lithological types (dip and strike of rock layers). Surfaces approximation for strata surfaces. Creation 2D and 3D models of the geological situation.<br \/>\n<strong>Findings. <\/strong>This approach is rapid and suitable for fast analysis of large areas without field investigations. Unlike the traditional way of orientation geological features finding In Situ, this approach can avoid personal errors on account of the statistical significance of points quantity. The disadvantages are impossibility explore territories with vegetation and\/or smooth relief. But this is a problem of all approaches which are based on\u00a0 remote sensing data in geology.<\/p>\n<p style=\"text-align: justify\"><strong>Keywords:<\/strong> remote sensing data, geoinformation system (GIS), dip line, strike line, dip azimuth, trend azimuth.<\/p>\n<p>&nbsp;<\/p>\n<p style=\"text-align: justify\"><span style=\"color: #0000ff\"><em><strong><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2021\/05\/\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430_1_2019-\u0424\u0406\u041d\u0406\u0428-58-61_\u0422\u0406\u0428\u0410\u0404\u0412.pdf\"><span style=\"color: #0000ff\">The full text of papers <\/span><\/a> <\/strong><\/em><\/span><\/p>\n<p>&nbsp;<\/p>\n<p style=\"text-align: justify\"><strong>References <\/strong><\/p>\n<ol>\n<li style=\"text-align: justify\">Baghatospektraljni metody dystancijnogho zonduvannja Zemli v zadachakh pryrodokorystuvannja: monoghrafija [za red. V.I. Ljaljka, M.O.Popova]. \u2013 K.: Nauk. dumka, 2006. \u2013 360 s.<\/li>\n<li style=\"text-align: justify\">Zheleznjak O.O. Kosmichni ta gheoinformacijni systemy \/ O.O. Zheleznjak, V.I. Zacerkovnyj, V.S. Kysljuk, O.Je. Nikolajenko. \u2013 Nizhyn: Vyd-vo Nizhyn. derzh. un-tu im. M. Ghogholja, 2016. \u2013 374 s.<\/li>\n<li style=\"text-align: justify\">Zhukov M.N. Matematychna statystyka ta obrobka gheologhichnykh danykh: pidruchnyk \/ M.N. Zhukov. \u00ac\u2013 K.: Vydavn.-polighr. centr \u201cKyjivsjkyj universytet\u201d, 2008. \u2013 518 s.<\/li>\n<li style=\"text-align: justify\">Zacerkovnyj V.I. Gheoinformacijni systemy v naukakh pro Zemlju \/ V.I. Zacerkovnyj, I.V. Tishajev, V.K. Demydov. \u2013 Nizhyn: Vyd-vo Nizhyn. derzh. un-tu im. M. Ghogholja, 2016. \u2013 510 s.<\/li>\n<li style=\"text-align: justify\">Petrusevich M.N. Aerometody pri geologicheskikh issledovaniyakh \/ M.N. Petrusevich. \u2013 M.: Gosgeoltekhizdat, 1962. \u2013 408 s.<\/li>\n<li style=\"text-align: justify\">Pravilo Kramera. Metod obratnoy matritsy. \u2013 [Elektronniy resurs]. \u2012 Rezhim dostupa: http:\/\/www.mathprofi.ru\/pravilo_kramera_matrichnyi_metod.html (data zvernennya 07.12.2016).<\/li>\n<li style=\"text-align: justify\">Miller V.C. Photogeology \/ V.C. Miller. \u2013 McGraw-Hill Book Co., 1961. \u2013 245 p.<\/li>\n<li style=\"text-align: justify\">Schowengerdt R.A. Remote Sensing: Models and Methods for Image Processing. \u2012 Third ed. \/ R.A. Schowengerdt. \u2013 ELSEVIER, 2007. \u2013 515 p.<\/li>\n<li style=\"text-align: justify\">Silas T. ArcPy and ArcGIS \u2013 Geospatial Analysis with Python \/ T. Silas. \u2013 PACKT Publishing, 2015. \u2013 224 p.<\/li>\n<li style=\"text-align: justify\">SRTM Tile Grabber. \u2013 [Elektronniy resurs]. \u2012 Rezhim dostupu: http:\/\/dwtkns.com\/srtm\/ (data zvernennya 07.12.2016).<\/li>\n<\/ol>\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2019; 1(69) : 58-61 \u0423\u0414\u041a 528.88 (914\/919):629.783 THE APPROACH TO USE OF REMOTE SENSING DATA FOR DEFINITION THE DIP AND STRIKE OF ROCK LAYERS V.I. Zatserkovnyi\u00a0, I.V. Tishaiev, O.M. Pylypenko Taras Shevchenko National University of Kyiv, Institute of Geology, 90, Vasylkivska Str., Kyiv, 03022, Ukraine, e-mail: zvigis@mail.ru, ivantishaev@yandex.ru, ya.ne.haker@yandex.ua Purpose. It is investigated the approach to the use the remote sensing data for finding the dip and strike of rock layers. A geometric model for approximation surfaces of rock layers and finding spatial orientation elements, can be designed and deployed based on the remote sensing data. Design\/methodology\/approach. The methodology was implemented as workflow. Geological recognition (manual or automatized) of remote sensing data (optical range) consists of identification lithological types and tracing edge polylines between neighbors types. Automated extraction spatial information from Digital Elevation Model (DEM) for each vertex of edge polylines. Calculation spatial orientation elements of surfaces for each conjunction of\u00a0 lithological types (dip and strike of rock layers). Surfaces approximation for strata surfaces. Creation 2D and 3D models of the geological situation. Findings. This approach is rapid and suitable for fast analysis of large areas without field investigations. Unlike the traditional way of orientation geological features finding In Situ, this approach can avoid personal errors on account of the statistical significance of points quantity. The disadvantages are impossibility explore territories with vegetation and\/or smooth relief. But this is a problem of all approaches which are based on\u00a0 remote sensing data in geology. Keywords: remote sensing data, geoinformation system (GIS), dip line, strike line, dip azimuth, trend azimuth. &nbsp; The full text of papers &nbsp; References Baghatospektraljni metody dystancijnogho zonduvannja Zemli v zadachakh pryrodokorystuvannja: monoghrafija [za red. V.I. Ljaljka, M.O.Popova]. \u2013 K.: Nauk. dumka, 2006. \u2013 360 s. Zheleznjak O.O. Kosmichni ta gheoinformacijni systemy \/ O.O. Zheleznjak, V.I. Zacerkovnyj, V.S. Kysljuk, O.Je. Nikolajenko. \u2013 Nizhyn: Vyd-vo Nizhyn. derzh. un-tu im. M. Ghogholja, 2016. \u2013 374 s. Zhukov M.N. Matematychna statystyka ta obrobka gheologhichnykh danykh: pidruchnyk \/ M.N. Zhukov. \u00ac\u2013 K.: Vydavn.-polighr. centr \u201cKyjivsjkyj universytet\u201d, 2008. \u2013 518 s. Zacerkovnyj V.I. Gheoinformacijni systemy v naukakh pro Zemlju \/ V.I. Zacerkovnyj, I.V. Tishajev, V.K. Demydov. \u2013 Nizhyn: Vyd-vo Nizhyn. derzh. un-tu im. M. Ghogholja, 2016. \u2013 510 s. Petrusevich M.N. Aerometody pri geologicheskikh issledovaniyakh \/ M.N. Petrusevich. \u2013 M.: Gosgeoltekhizdat, 1962. \u2013 408 s. Pravilo Kramera. Metod obratnoy matritsy. \u2013 [Elektronniy resurs]. \u2012 Rezhim dostupa: http:\/\/www.mathprofi.ru\/pravilo_kramera_matrichnyi_metod.html (data zvernennya 07.12.2016). Miller V.C. Photogeology \/ V.C. Miller. \u2013 McGraw-Hill Book Co., 1961. \u2013 245 p. Schowengerdt R.A. Remote Sensing: Models and Methods for Image Processing. \u2012 Third ed. \/ R.A. Schowengerdt. \u2013 ELSEVIER, 2007. \u2013 515 p. Silas T. ArcPy and ArcGIS \u2013 Geospatial Analysis with Python \/ T. Silas. \u2013 PACKT Publishing, 2015. \u2013 224 p. SRTM Tile Grabber. \u2013 [Elektronniy resurs]. \u2012 Rezhim dostupu: http:\/\/dwtkns.com\/srtm\/ (data zvernennya 07.12.2016).<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-7665","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.9 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>- \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\/7665-2\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" 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:description\" content=\"Geoinformatika 2019; 1(69) : 58-61 \u0423\u0414\u041a 528.88 (914\/919):629.783 THE APPROACH TO USE OF REMOTE SENSING DATA FOR DEFINITION THE DIP AND STRIKE OF ROCK LAYERS V.I. Zatserkovnyi\u00a0, I.V. Tishaiev, O.M. Pylypenko Taras Shevchenko National University of Kyiv, Institute of Geology, 90, Vasylkivska Str., Kyiv, 03022, Ukraine, e-mail: zvigis@mail.ru, ivantishaev@yandex.ru, ya.ne.haker@yandex.ua Purpose. It is investigated the approach to the use the remote sensing data for finding the dip and strike of rock layers. A geometric model for approximation surfaces of rock layers and finding spatial orientation elements, can be designed and deployed based on the remote sensing data. Design\/methodology\/approach. The methodology was implemented as workflow. Geological recognition (manual or automatized) of remote sensing data (optical range) consists of identification lithological types and tracing edge polylines between neighbors types. Automated extraction spatial information from Digital Elevation Model (DEM) for each vertex of edge polylines. Calculation spatial orientation elements of surfaces for each conjunction of\u00a0 lithological types (dip and strike of rock layers). Surfaces approximation for strata surfaces. Creation 2D and 3D models of the geological situation. Findings. This approach is rapid and suitable for fast analysis of large areas without field investigations. Unlike the traditional way of orientation geological features finding In Situ, this approach can avoid personal errors on account of the statistical significance of points quantity. The disadvantages are impossibility explore territories with vegetation and\/or smooth relief. But this is a problem of all approaches which are based on\u00a0 remote sensing data in geology. Keywords: remote sensing data, geoinformation system (GIS), dip line, strike line, dip azimuth, trend azimuth. &nbsp; The full text of papers &nbsp; References Baghatospektraljni metody dystancijnogho zonduvannja Zemli v zadachakh pryrodokorystuvannja: monoghrafija [za red. V.I. Ljaljka, M.O.Popova]. \u2013 K.: Nauk. dumka, 2006. \u2013 360 s. Zheleznjak O.O. Kosmichni ta gheoinformacijni systemy \/ O.O. Zheleznjak, V.I. Zacerkovnyj, V.S. Kysljuk, O.Je. Nikolajenko. \u2013 Nizhyn: Vyd-vo Nizhyn. derzh. un-tu im. M. Ghogholja, 2016. \u2013 374 s. Zhukov M.N. Matematychna statystyka ta obrobka gheologhichnykh danykh: pidruchnyk \/ M.N. Zhukov. \u00ac\u2013 K.: Vydavn.-polighr. centr \u201cKyjivsjkyj universytet\u201d, 2008. \u2013 518 s. Zacerkovnyj V.I. Gheoinformacijni systemy v naukakh pro Zemlju \/ V.I. Zacerkovnyj, I.V. Tishajev, V.K. Demydov. \u2013 Nizhyn: Vyd-vo Nizhyn. derzh. un-tu im. M. Ghogholja, 2016. \u2013 510 s. Petrusevich M.N. Aerometody pri geologicheskikh issledovaniyakh \/ M.N. Petrusevich. \u2013 M.: Gosgeoltekhizdat, 1962. \u2013 408 s. Pravilo Kramera. Metod obratnoy matritsy. \u2013 [Elektronniy resurs]. \u2012 Rezhim dostupa: http:\/\/www.mathprofi.ru\/pravilo_kramera_matrichnyi_metod.html (data zvernennya 07.12.2016). Miller V.C. Photogeology \/ V.C. Miller. \u2013 McGraw-Hill Book Co., 1961. \u2013 245 p. Schowengerdt R.A. Remote Sensing: Models and Methods for Image Processing. \u2012 Third ed. \/ R.A. Schowengerdt. \u2013 ELSEVIER, 2007. \u2013 515 p. Silas T. ArcPy and ArcGIS \u2013 Geospatial Analysis with Python \/ T. Silas. \u2013 PACKT Publishing, 2015. \u2013 224 p. 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Zatserkovnyi\u00a0, I.V. Tishaiev, O.M. Pylypenko Taras Shevchenko National University of Kyiv, Institute of Geology, 90, Vasylkivska Str., Kyiv, 03022, Ukraine, e-mail: zvigis@mail.ru, ivantishaev@yandex.ru, ya.ne.haker@yandex.ua Purpose. It is investigated the approach to the use the remote sensing data for finding the dip and strike of rock layers. A geometric model for approximation surfaces of rock layers and finding spatial orientation elements, can be designed and deployed based on the remote sensing data. Design\/methodology\/approach. The methodology was implemented as workflow. Geological recognition (manual or automatized) of remote sensing data (optical range) consists of identification lithological types and tracing edge polylines between neighbors types. Automated extraction spatial information from Digital Elevation Model (DEM) for each vertex of edge polylines. Calculation spatial orientation elements of surfaces for each conjunction of\u00a0 lithological types (dip and strike of rock layers). Surfaces approximation for strata surfaces. Creation 2D and 3D models of the geological situation. Findings. This approach is rapid and suitable for fast analysis of large areas without field investigations. Unlike the traditional way of orientation geological features finding In Situ, this approach can avoid personal errors on account of the statistical significance of points quantity. The disadvantages are impossibility explore territories with vegetation and\/or smooth relief. But this is a problem of all approaches which are based on\u00a0 remote sensing data in geology. Keywords: remote sensing data, geoinformation system (GIS), dip line, strike line, dip azimuth, trend azimuth. &nbsp; The full text of papers &nbsp; References Baghatospektraljni metody dystancijnogho zonduvannja Zemli v zadachakh pryrodokorystuvannja: monoghrafija [za red. V.I. Ljaljka, M.O.Popova]. \u2013 K.: Nauk. dumka, 2006. \u2013 360 s. Zheleznjak O.O. Kosmichni ta gheoinformacijni systemy \/ O.O. Zheleznjak, V.I. Zacerkovnyj, V.S. Kysljuk, O.Je. Nikolajenko. \u2013 Nizhyn: Vyd-vo Nizhyn. derzh. un-tu im. M. Ghogholja, 2016. \u2013 374 s. Zhukov M.N. Matematychna statystyka ta obrobka gheologhichnykh danykh: pidruchnyk \/ M.N. Zhukov. \u00ac\u2013 K.: Vydavn.-polighr. centr \u201cKyjivsjkyj universytet\u201d, 2008. \u2013 518 s. Zacerkovnyj V.I. Gheoinformacijni systemy v naukakh pro Zemlju \/ V.I. Zacerkovnyj, I.V. Tishajev, V.K. Demydov. \u2013 Nizhyn: Vyd-vo Nizhyn. derzh. un-tu im. M. Ghogholja, 2016. \u2013 510 s. Petrusevich M.N. Aerometody pri geologicheskikh issledovaniyakh \/ M.N. Petrusevich. \u2013 M.: Gosgeoltekhizdat, 1962. \u2013 408 s. Pravilo Kramera. Metod obratnoy matritsy. \u2013 [Elektronniy resurs]. \u2012 Rezhim dostupa: http:\/\/www.mathprofi.ru\/pravilo_kramera_matrichnyi_metod.html (data zvernennya 07.12.2016). Miller V.C. Photogeology \/ V.C. Miller. \u2013 McGraw-Hill Book Co., 1961. \u2013 245 p. Schowengerdt R.A. Remote Sensing: Models and Methods for Image Processing. \u2012 Third ed. \/ R.A. Schowengerdt. \u2013 ELSEVIER, 2007. \u2013 515 p. Silas T. ArcPy and ArcGIS \u2013 Geospatial Analysis with Python \/ T. Silas. \u2013 PACKT Publishing, 2015. \u2013 224 p. 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