BELTS OF ARID AND HUMID SEDIMENTATION DURING THE CONIACIAN-MAASTRICHTIAN AGES OF THE LATE CRETACEOUS

dc.contributor.authorZharkov M.A.
dc.date.accessioned2020-12-31T03:46:34Z
dc.date.available2020-12-31T03:46:34Z
dc.date.issued1998
dc.description.abstractThe existence of six climatic belts - northern circumpolar humid coal, northern mid-latitude coal-bauxite-kaolinite, northern arid tropical-subtropical evaporite, equatorial humid coal-bauxite-kaolinite, southern arid tropical-subtropical evaporite, and southern humid coal-bauxite-kaolinite - are substantiated. Regular secular variations in latitudinal position of arid and humid belts related to global climate warming and general humidization at the end of the Late Cretaceous epoch are outlined.
dc.identifierhttps://elibrary.ru/item.asp?id=13305498
dc.identifier.citationStratigraphy and Geological Correlation, 1998, , 5, 429-439
dc.identifier.issn0869-5938
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/21882
dc.subjectConiacianen
dc.subject.ageМезозой::Меловаяru
dc.titleBELTS OF ARID AND HUMID SEDIMENTATION DURING THE CONIACIAN-MAASTRICHTIAN AGES OF THE LATE CRETACEOUS
dc.typeСтатья

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