Abstract
Special features of distribution of seismic waves propagation velocity in the Earth crust in the area of uranium deposits (Kirovograd ore area of Ingul megablock of the Ukrainian Shield)
Highlights
Íà òåðèòîð3¿ Ê3ðîâîãðàäñüêîãî ðóäíîãî ðàéîíó (ÊÐÐ) âèêîíàíî âåëèêèé îáñÿã ðåã3îíàëüíèõ ãåîô3çè÷íèõ äîñë3äæåíü ìåòîäîì ãëèáèííîãî ñåéñì3÷íîãî çîíäóâàííÿ (ÃÑÇ)
Âèÿâëåíî ñêëàäí ñï3ââ3äíîøåííÿ ì3æ øâèäêîñòÿìè ó çåìí3é êîð ðîäîâèù óðàíó òà íà ä3ëÿíêàõ ïîçà íèìè
Íà ãëèáèíàõ 04 êì øâèäêîñò íà ðîäîâèùàõ óðàíó âèù
Summary
Íà òåðèòîð3¿ Ê3ðîâîãðàäñüêîãî ðóäíîãî ðàéîíó (ÊÐÐ) âèêîíàíî âåëèêèé îáñÿã ðåã3îíàëüíèõ ãåîô3çè÷íèõ äîñë3äæåíü ìåòîäîì ãëèáèííîãî ñåéñì3÷íîãî çîíäóâàííÿ (ÃÑÇ). 1. Êàðòà 3çîë3í3é ΔV íà ãëèáèííèõ ïåðåð3çàõ 1, 2, 3 3 4 êì ó ðàéîí[3] ðîçì3ùåííÿ óðàíîâèõ ðîäîâèù: 1 3çîë3í3¿ ΔV, êì/ñ; 2 òðàíñðåã3îíàëüíà çîíà ðîçòÿãó ÕåðñîíÑìîëåíñüê; 3 çîíè ðîçëîì3â (1 Ê3ðîâîãðàäñüêà, 2 Ñóáîòñüêî-Ìîøîðèíñüêà, 3 Çâåíèãîðîäñüêî-Áðàòñüêà); 4 ïðîô3ëü ÃÑÇ; 5 ãåîòðàâåðñ ÃÑÇ; 6 ðîäîâèùà óðàíó; 7 ðîäîâèùà óðàíó, äëÿ ÿêèõ íàâåäåíî ãåîëîã3÷í3 ðîçð3çè [Ñòàðîñòåíêî è äð., 2010, 2011] ( Âàòóòèíñüêå, Ï Ïàðòèçàíñüêå, Í Íîâîêîñòÿíòèí3âñüêå, Ñ Ñåâåðèíñüêå, Ì Ì3÷óðèíñüêå); 8 êîíòóð ãåîëîã3÷íî¿ ñòðóêòóðè (ÊÍÏ Êîðñóíü-Íîâîìèðãîðîäñüêèé ïëóòîí, ÍÓÌ Íîâîóêðà¿íñüêèé ìàñèâ). Öå ïîòðåáóo äîäàòêîâîãî âèâ÷åííÿ, à ñàìå îêðåìîãî âèçíà÷åííÿ ì3ðè â3äõèëåííÿ â3ä íîðìàëüíèõ øâèäêîñòåé ó á3ê ¿õ çíèæåííÿ (äåô3öèò øâèäêîñòåé) ó çåìí3é êîð[3] ÿê íà öèõ ðîäîâèùàõ, òàê 3 íà ä3ëÿíêàõ ïîçà íèìè.
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