Ââåäåíèå Âûäåëåíèå ðàçëîìíûõ çîí íà ìåñòíîñòè èìååò ñóùåñòâåííîå ïðàêòè-÷åñêîå çíà÷åíèå äëÿ îïðåäåëåíèÿ ãðàíèö ðàñïðîñòðàíåíèÿ ñâÿçàííûõ ñ íèìè çåìëåòðÿñåíèé, ðóäîïðîÿâëåíèé, ìåñòîðîaeäåíèé óãëåâîäîðîäîâ è ò. ä. Äëÿ áîëüøèíñòâà ðåãèîíîâ âûäåëåíèå ðàçëîìîâ ïðÿìûìè ìåòîäàìè íåâîçìîaeíî èç-çà ñëàáîé îáíàaeåííîñòè êîðåííûõ ïîðîä. Ïîýòîìó äëÿ èõ èçó÷åíèÿ íà ïåðâîå ìåñòî âûõîäÿò ãåîôèçè÷åñêèå ìåòîäû. Íåñîìíåííî, íàèáîëåå íàäåaeíûìè ÿâëÿþòñÿ ñåéñ-ìè÷åñêèå ìåòîäû, îäíàêî íå âñåãäà

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For the Timan-Severouralsk region and adjacent territories, the possibility of using radon survey for mapping fault zones has been considered.The complex of studies also included the study of potential fields, materials of seismic methods.The faults of the Kirovsko-Kazhimsky and Pechora-Kolvinsky aulacogens, the Vychegodskydepression and the Timan ridge have been studied.The schemes of distribution of radon fields within the fault zones have been compiled. The nature of the distribution of the volumetric activity of radon over kimberlite pipes has been investigated on the territory of Central Timan.The observed increase of the radon level over pipes can be an additional prospecting indicator. The book can be useful for specialists studying tectonic zoning, as well as geologists and geophysicists working in various fields of earth sciences.

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23The scheme of the fault tectonics of the Pechora-Kolva aulakogen was constructed on the basis of the interpretation of seismic data, an updated scheme of the fault tectonics of the Pechora-Kolvich aulakogen was constructed; kinematics, morphology and occurrence of deep tectonic deformation in the radon field were studied. The results of the research show that the faults are characterized by a complex internal structure, variability of kinematics at different sites, both in the longitudinal and transverse directions. The faults of the western side of the aulakogen and the Upper Pechora depression clearly occur in the radon field by high values of the volume radon activity. : aulakogen, faults, kinematics, morphology, radon survey. ÓÄÊ 551.243, 550.389.1 DOI: 10.19110/2221: aulakogen, faults, kinematics, morphology, radon survey. ÓÄÊ 551.243, 550.389.1 DOI: 10.19110/ -1381: aulakogen, faults, kinematics, morphology, radon survey. ÓÄÊ 551.243, 550.389.1 DOI: 10.19110/ -2017 ËÎÊÀËÈÇÀÖÈß ezimova89@mail.ru; udoratin@geo.komisc.ru; asmagomedova@geo.komisc.ru Íà îñíîâå èíòåðïðåòàöèè ñåéñìè÷åñêèõ äàííûõ áûëà ïîñòðîåíà îáíîâëåííàÿ ñõåìà ðàçëîìíîé òåêòîíèêè Ïå÷î-ðî-Êîëâèíñêîãî àâëàêîãåíà; èçó÷åíû êèíåìàòèêà, ìîðôîëîãèÿ è ïðîÿâëåíèå â ïîëå ðàäîíà ãëóáèííûõ òåêòîíè÷åñêèõ íàðóøåíèé. Ðåçóëüòàòû èññëåäîâàíèé ïîêàçàëè, ÷òî äèçúþíêòèâû õàðàêòåðèçóþòñÿ ñëîaeíûì âíóòðåííèì ñòðîåíèåì, èçìåí÷èâîñòüþ êèíåìàòèêè íà ðàçíûõ ó÷àñòêàõ êàê â ïðîäîëüíîì, òàê è â ïîïåðå÷íîì íàïðàâëåíèè. Ðàçðûâíûå íàðóøå-íèÿ çàïàäíîãî áîðòà àâëàêîãåíà è Âåðõíåïå÷îðñêîé âïàäèíû îò÷åòëèâî ïðîÿâëÿþòñÿ â ïîëå ðàäîíà âûñîêèìè çíà÷åíè-ÿìè îáúåìíîé àêòèâíîñòè ðàäîíà. Keywords ÂâåäåíèåÍà îñíîâå èññëåäîâàíèé, ïðîâåäåííûõ â èíñòèòóòå ãåîëîãèè Êîìè ÍÖ ÓðÎ ÐÀÍ, óñòàíîâëåíî, ÷òî íåêîòî-ðûå ñòðóêòóðû Òèìàíî-Ïå÷îðñêîé ïëèòû, â ÷àñòíîñòè Ïå÷îðî-Êîëâèíñêèé àâëàêîãåí (ÏÊÀ), îòíîñÿòñÿ ê îïàñ-íûì â ñåéñìè÷åñêîì îòíîøåíèè ðåãèîíàì. Àíàëèç êîìï-ëåêñà ãåîëîãî-ãåîôèçè÷åñêèõ äàííûõ ïî ãëóáèííîìó ñòðî-åíèþ ðåãèîíà, äèçúþíêòèâíîé òåêòîíèêå, íåîòåêòîíè÷åñ-êîé àêòèâíîñòè è ìåñòîïîëîaeåíèþ èçâåñòíûõ î÷àãîâ çåì-ëåòðÿñåíèé ïîçâîëèë âûÿâèòü íåêîòîðûå îñîáåííîñòè ðàçìåùåíèÿ ýòèõ î÷àãîâ [1]. Ïîçäíåå ïî ðåçóëüòàòàì êîì-ïëåêñíîãî èññëåäîâàíèÿ è ïî èñòîðè÷åñêèì äàííûì î çåì-ëåòðÿñåíèÿõ áûëà ïîñòðîåíà ñõåìà ñåéñìè÷åñêîãî ðàéî-íèðîâàíèÿ Åâðîïåéñêîãî Ñåâåðî-Âîñòîêà, ãäå âûäåëÿþò-ñÿ Êèðîâñêî-Êàaeèìñêàÿ, Ìåçåíñêî-Âàøêèíñêàÿ è Ïðè-ïå÷îðñêàÿ çîíû ñåéñìè÷åñêîé àêòèâíîñòè [3].  ïðåäåëàõ ïîñëåäíåé ðàíåå áûëè çàðåãèñòðèðîâàíû íåñêîëüêî çåì-ëåòðÿñåíèé, âîçìîaeíûå î÷àãè (ÂÎÇ) êîòîðûõ ïðèóðî÷å-íû ê ãëóáèííûì ðàçëîìàì çàïàäíîãî áîðòà Ïå÷îðî-Êîë-âèíñêîãî àâëàêîãåíà.Âûäåëåíèå ðàçëîìíûõ çîí íà ìåñòíîñòè èìååò ñóùå-ñòâåííîå ïðàêòè÷åñêîå çíà÷åíèå äëÿ îïðåäåëåíèÿ ãðàíèö ðàñïðîñòðàíåíèÿ ñâÿçàííûõ ñ íèìè çåìëåòðÿñåíèé, à òàê-aeå ðóäîïðîÿâëåíèé è ìåñòîðîaeäåíèé óãëåâîäîðîäîâ, ïî-ýòîìó öåëü íàøåãî èññëåäîâàíèÿ çàêëþ÷àåòñÿ â ïîñòðîå-íèè äåòàëüíîé ñõåìû ðàçëîìíîé òåêòîíèêè äëÿ òåððèòî-ðèè Ïå÷îðî-Êîëâèíñêîãî àâëàêîãåíà è áëèçëåaeàùèõ ïëî-ùàäåé.  ñîîòâåòñòâèè ñ öåëüþ ïåðåä ðàáîòîé ïîñòàâëåíû ñëåäóþùèå çàäà÷è...