Overview

V knige, na osnovanii novykh dannykh, poluchennykh v protsesse geologicheskogo kartirovaniya, rassmotreny geologicheskoe stroenie, litostratigrafiya, zonal'noe delenie po melkim foraminiferam, usloviya sedimentatsii i formirovaniya paleotsenovo - eotsenovogo flisha Ukrainskikh Vneshnikh Karpat v kontekste razvitiya akkretsionnoy prizmy Flishevykh Karpat. Utochneny vozrast i pokazan diakhronnyy kharakter granits bol'shinstva svit paleotsena i eotsena, stratifitsirovany ranee prakticheski neraschlenennye dooligotsenovye obrazovaniya Silezskoy (Krosnenskoy) i Svidovetskoy tektonicheskikh edinits. Vpervye predlozhena biozonal'naya stratifikatsiya paleotsena i eotsena Ukrainskikh Karpat po agglyutiniruyushchim foraminiferam, kotorye rezko preobladayut libo imeyut isklyuchitel'noe razvitie vo flishe. Sdelan vyvod, chto bol'shaya chast' paleotsenovo-eotsenovykh osadkov Karpatskogo flishevogo basseyna otlagalas' v rezul'tate turbiditnoy i (gemi)pelagicheskoy sedimentatsii v oblasti nizhney batiali-abissali nizhe ili blizko urovnya karbonatnoy kompensatsii. Izobrazheny i opisany pyat'desyat vidov foraminifer, preimushchestvenno iz otlozheniy Silezskogo i Svidovetskogo pokrovov.

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