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Please use this identifier to cite or link to this item: https://elib.bsu.by/handle/123456789/247375
Title: Палеорельеф дна бассейна кузьмичевского возраста южной части Припятского палеорифта
Authors: Обровец, С. М.
Демидович, Л. А.
Коробчук, Л. А.
Issue Date: 1996
Publisher: Минск : Універсітэцкае
Citation: Вестник Белорусского государственного университета. Сер. 2, Химия. Биология. География. – 1996. – № 1. – С. 53-57.
Abstract: Nine Iithological and facial fields are distinguished in the Upper Famenian Kusmichevian deposits according to the changes in the thicknesses, Iithological compositions, structural and textural features of rocks. Positive and negative forms of bottom paleorelief were recognized from investigations carried out. There are islands, island slopes, submarine rises and submarine ridges deltaic paleotracts. Paleovalleys were the main negative forms of the paleorelief
URI: https://elib.bsu.by/handle/123456789/247375
ISSN: 0372-5340
Licence: info:eu-repo/semantics/openAccess
Appears in Collections:1996, №1 (февраль)

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