Приказ основних података о документу

dc.creatorĐurović, Predrag
dc.date.accessioned2021-09-24T15:17:17Z
dc.date.available2021-09-24T15:17:17Z
dc.date.issued2009
dc.identifier.issn1581-6613
dc.identifier.urihttps://gery.gef.bg.ac.rs/handle/123456789/296
dc.description.abstractMount Durmitor is situated in the southeastern part of the Dinaric mountain system in Montenegro. Throughout the Pleistocene there were many glaciers there, which descended to adjacent karst plateau. Types of glaciers, their number and direction of moving were mostly affected by geological structure (carbonate basis) and pre-glacial relief (karst and fluvial relief). During two phases of intensive glaciation, the surface that had been seized by glacial changes also changed. Over 54% of the surface of Durmitor was exposed to the glacial process of the stronger phase and about 36% of the weaker phase. Cirque type of glaciation dominated the third phase.en
dc.publisherLjubljana: Geografski inštitut Antona Melika ZRC SAZU
dc.rightsopenAccess
dc.sourceActa Geographica Slovenica - Geografski zbornik
dc.subjectgeographyen
dc.subjectglaciationen
dc.subjectglacier reconstructionen
dc.subjectPleistoceneen
dc.subjectDurmitoren
dc.subjectDinaric mountainsen
dc.subjectMontenegroen
dc.titleReconstruction of the pleistocene glaciers of mount Durmitor in Montenegroen
dc.typearticle
dc.rights.licenseARR
dcterms.abstractЂуровић, Предраг;
dc.citation.volume49
dc.citation.issue2
dc.citation.spage263
dc.citation.epage279
dc.citation.other49(2): 263-279
dc.citation.rankM22
dc.identifier.wos000272997500002
dc.identifier.doi10.3986/AGS49202
dc.identifier.scopus2-s2.0-75149145896
dc.identifier.fulltexthttps://gery.gef.bg.ac.rs/bitstream/id/262/294.pdf
dc.identifier.rcubhttps://hdl.handle.net/21.15107/rcub_gery_296
dc.type.versionpublishedVersion


Документи

Thumbnail

Овај документ се појављује у следећим колекцијама

Приказ основних података о документу