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Пðîвåдåíî кîìпëåкñíîå ëèòîëîãè÷åñкîå è ìèкðîпàëåîíòîëîãè÷åñкîå (дèàòîìîвый è пàëèíîëîãè÷åñкèй àíàëèзы) èзó÷åíèå, ðàдèîóãëåðîдíîå дàòèðîвàíèå ñòðàòèфèöèðîвàííых дîííых îòëîжåíèй, фîðìèðóющèх фàöèàëьíî ðàзíîðîдíыå îñàдî÷íыå òîëщè в èзîëèðîвàííîй кîòëîвèíå ìàëîãî îзåðà, ðàñпîëîжåííîãî в пðåдåëàх Êîëвèöкîãî ãðàбåíà íà îñòðîвå Îëåíèй в Êàíдàëàкшñкîì зàëèвå Бåëîãî ìîðя. Óñòàíîвëåíî, ÷òî ñòðàòèãðàфèя фàöèàëьíî ðàзíîðîдíых òîëщ в èзó÷åííîì вîдîåìå ñвязàíà ñ пîздíåãîëîöåíîвîй ðåãðåññèåй ìîðя. Ðàдèîóãëåðîдíîå дàòèðîвàíèå фàöèàëьíых пåðåхîдîв пîзвîëèëî îпðåдåëèòь вðåìя èзîëяöèè îзåðíîй дåпðåññèè îò ìîðя. Óñòàíîвëåíî, ÷òî ñкîðîñòь пîдíяòèя зåìíîй пîвåðхíîñòè в ðàйîíå èññëåдîвàííîãî îзåðà зíà÷èòåëьíî вышå ñкîðîñòåй пîдíяòèя îзåð ñ òàкèìè жå выñîòíыìè îòìåòкàìè íà бåðåãàх Êàíдàëàкшñкîãî зàëèвà. Эòî ñвязàíî ñ дèффåðåíöèðîвàííыìè íåîòåкòîíè÷åñкèìè двèжåíèяìè ìîðфîòåкòîíè÷åñкèх бëîкîв. Êëю÷åвыå ñëîвà: Кàíäàлàкшскèй çàлèв, ìàлîå îçåðî, äîííыå îтлîжåíèя, гîлîöåí, лèтîлîгèя, ìèкðîпàлåîíтîлîгèя, íåîтåктîíèкà.

Lithology and micro-paleontology of small lake bottom sediments of the Oleniy Island in Kandalaksha Bay of the White Sea