Abstract
The results of two-dimensional inversion of magnetoteluric data, focused along the DSS profile Novoazovsk—Titovka have been presented. On the territory of Donbas two objects have been distinguished with low resistance (causing Donbass conductivity anomaly) which occur: in the southern part in sedimentary rocks (at a depth of 1—10 km), in the central part (at a depth of 1—18 km) in sedimentary rocks and penetrating into consolidated crust. Total cumulative integral conductivity of the objects is about 3×108 S×m. The most reliably the objects spatially correlate with the coal-bearing rocks of the Carboniferous.
Highlights
Çàäà÷à íàñòîÿùåé ðàáîòû ïîñòðîåíèå ãåîýëåêòðè÷åñêîé ìîäåëè âäîëü ïðîôèëÿ ÃÑÇ XI ñ ïîìîùüþ ÷èñëåííîãî ìîäåëèðîâàíèÿ (îáðàòíàÿ çàäà÷à) ñ èñïîëüçîâàíèåì íîâûõ äàííûõ, ïîëó÷åííûõ ñîâðåìåííûìè öèôðîâûìè ñòàíöèÿìè â 15 ïóíêòàõ íà ýòîì ïðîôèëå.
Ïðè ýòîì íåîáõîäèìî ó÷åñòü, ÷òî íàèáîëåå òî÷íûå çíà÷åíèÿ àçèìóòîâ îïðåäåëÿþòñÿ â õàðàêòåðíûõ ÷àñòÿõ ïðîôèëÿ, êîòîðûå óêàçàíû âûøå, íàä äâóìåðíîé àíîìàëèåé ïðîâîäÿùåãî îáúåêòà.
Òîðûõ ïðèâåäåíî íèæå) ñ ó÷åòîì ðåçóëüòàòîâ èíòåðïðåòàöèè ìàãíèòîòåëëóðè÷åñêèõ äàííûõ âäîëü ñåéñìè÷åñêîãî ïðîôèëÿ ÃÑÇ X [Ëîãâèíîâ, Ëûñåíêî, 1995] è êàðòû ñóììàðíîé ïðîäîëüíîé ïðîâîäèìîñòè ÄÄ [Ëîãâèíîâ, 2002]; ãåîýëåêòðè÷åñêèå ïàðàìåòðû äëÿ êðèñòàëëè÷åñêèõ ïîðîä çåìíîé êîðû è âåðõíåé ìàíòèè áûëè èñïîëüçîâàíû ïî ðåçóëüòàòàì èíâåðñèè êðèâîé èíäóêöèîííîãî çîíäèðîâàíèÿ íà ãåîìàãíèòíîé îáñåðâàòîðèè Êèåâ [Semenov et al, 2008].
Summary
Çàäà÷à íàñòîÿùåé ðàáîòû ïîñòðîåíèå ãåîýëåêòðè÷åñêîé ìîäåëè âäîëü ïðîôèëÿ ÃÑÇ XI ñ ïîìîùüþ ÷èñëåííîãî ìîäåëèðîâàíèÿ (îáðàòíàÿ çàäà÷à) ñ èñïîëüçîâàíèåì íîâûõ äàííûõ, ïîëó÷åííûõ ñîâðåìåííûìè öèôðîâûìè ñòàíöèÿìè â 15 ïóíêòàõ íà ýòîì ïðîôèëå. Ïðè ýòîì íåîáõîäèìî ó÷åñòü, ÷òî íàèáîëåå òî÷íûå çíà÷åíèÿ àçèìóòîâ îïðåäåëÿþòñÿ â õàðàêòåðíûõ ÷àñòÿõ ïðîôèëÿ, êîòîðûå óêàçàíû âûøå, íàä äâóìåðíîé àíîìàëèåé ïðîâîäÿùåãî îáúåêòà. Òîðûõ ïðèâåäåíî íèæå) ñ ó÷åòîì ðåçóëüòàòîâ èíòåðïðåòàöèè ìàãíèòîòåëëóðè÷åñêèõ äàííûõ âäîëü ñåéñìè÷åñêîãî ïðîôèëÿ ÃÑÇ X [Ëîãâèíîâ, Ëûñåíêî, 1995] è êàðòû ñóììàðíîé ïðîäîëüíîé ïðîâîäèìîñòè ÄÄ [Ëîãâèíîâ, 2002]; ãåîýëåêòðè÷åñêèå ïàðàìåòðû äëÿ êðèñòàëëè÷åñêèõ ïîðîä çåìíîé êîðû è âåðõíåé ìàíòèè áûëè èñïîëüçîâàíû ïî ðåçóëüòàòàì èíâåðñèè êðèâîé èíäóêöèîííîãî çîíäèðîâàíèÿ íà ãåîìàãíèòíîé îáñåðâàòîðèè Êèåâ [Semenov et al, 2008].
Sign-in/Register to view highlights & summary Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
