FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2807339920> ?p ?o ?g. }

• W2807339920 abstract "In this paper geological settings and geomorphological processes at the areas of two river catchments basins in Primorsko-Goranska County (in the NE Adriatic coastal area of Croatia) are presented: the Rjecina river catchment and the Dubracina river catchment. Both areas are a part of a unique morphostructural unit Rjecina valley-Bakar Bay-Vinodol valley in which karstified carbonate rocks prevail. Paleogene siliciclastic sedimentary rock complex, i.e. flysch, has a form of squeezed synciline between carbonate rocks. Geological contacts between carbonate and flysch rock mass are tectonic reverse faults, but with different mechanisms of origin. Neotectonic and recent tectonic movements caused irregular subsidence of flysch areas and the uplifting of the surrounding karstic terrain. Consequently, carbonate rock mass is placed on the top of the slopes, while the flysch crops out at the lower parts. Weathering processes cause disintegration of carbonate rock mass, separation of blocks and gravitational movement of rock blocks and debris over the flysch bedrock, as well as the accumulation of talus in the toe of rock scarps. Unlike carbonate rocks, flysch rock mass is more subjected to weathering with final product of soil type material. During the time, rock blocks and coarse grained fragments originating from the rockfalls were mixed with soil-like material from flysch weathered zone. These geomorphological processes produced potentially unstable slope deposits that are, in some areas, more than ten meters thick. Rockfalls from disintegrated carbonate scarps and sliding of talus are permanent geodyinamic phenomena. Energy of the relief was changing due to tectonic movements, as well as changes of local erosion base and the position of local riverbeds. Strong earthquakes could be also one of important triggering factors, because the investigated area is seismotectonicaly very active. The comparison of morphological evolution, as well as intensity and dimension of instabilities, shows a distinction between Rjecina valley and Vinodol valley, although both areas are a part of the same morphostructural unit. The recent rockfalls and rock sliding phenomena are frequent and intensive in the Rjecina valley. Some of these mass movements have huge dimensions. These instabilities are atypical for Adriatic area but also frequent in the Alps. Active talus is visible on the northwestern slope of the Vinodol valley. Extensive erosion processes are clearly visible in the central part of Vinodol valley: around of tributary streams of Dubracina river: Slani potok, Mala Dubracina and Kucina. The active and dormant landslides are situated in alteration with relatively stable part of slopes." @default.
• W2807339920 created "2018-06-13" @default.
• W2807339920 creator A5012441325 @default.
• W2807339920 creator A5032055941 @default.
• W2807339920 creator A5089898317 @default.
• W2807339920 date "2010-01-01" @default.
• W2807339920 modified "2023-09-26" @default.
• W2807339920 title "Geological and geomorphological conditions in the area of Rjecina river and Dubracina river cathcments (Primorsko-goranska county, Croatia)" @default.
• W2807339920 hasPublicationYear "2010" @default.
• W2807339920 type Work @default.
• W2807339920 sameAs 2807339920 @default.
• W2807339920 citedByCount "0" @default.
• W2807339920 crossrefType "journal-article" @default.
• W2807339920 hasAuthorship W2807339920A5012441325 @default.
• W2807339920 hasAuthorship W2807339920A5032055941 @default.
• W2807339920 hasAuthorship W2807339920A5089898317 @default.
• W2807339920 hasConcept C114679195 @default.
• W2807339920 hasConcept C114793014 @default.
• W2807339920 hasConcept C127313418 @default.
• W2807339920 hasConcept C137527640 @default.
• W2807339920 hasConcept C151730666 @default.
• W2807339920 hasConcept C17409809 @default.
• W2807339920 hasConcept C186295008 @default.
• W2807339920 hasConcept C191897082 @default.
• W2807339920 hasConcept C192562407 @default.
• W2807339920 hasConcept C19320362 @default.
• W2807339920 hasConcept C204665574 @default.
• W2807339920 hasConcept C2779452743 @default.
• W2807339920 hasConcept C2780659211 @default.
• W2807339920 hasConcept C40724407 @default.
• W2807339920 hasConcept C6494504 @default.
• W2807339920 hasConcept C77928131 @default.
• W2807339920 hasConceptScore W2807339920C114679195 @default.
• W2807339920 hasConceptScore W2807339920C114793014 @default.
• W2807339920 hasConceptScore W2807339920C127313418 @default.
• W2807339920 hasConceptScore W2807339920C137527640 @default.
• W2807339920 hasConceptScore W2807339920C151730666 @default.
• W2807339920 hasConceptScore W2807339920C17409809 @default.
• W2807339920 hasConceptScore W2807339920C186295008 @default.
• W2807339920 hasConceptScore W2807339920C191897082 @default.
• W2807339920 hasConceptScore W2807339920C192562407 @default.
• W2807339920 hasConceptScore W2807339920C19320362 @default.
• W2807339920 hasConceptScore W2807339920C204665574 @default.
• W2807339920 hasConceptScore W2807339920C2779452743 @default.
• W2807339920 hasConceptScore W2807339920C2780659211 @default.
• W2807339920 hasConceptScore W2807339920C40724407 @default.
• W2807339920 hasConceptScore W2807339920C6494504 @default.
• W2807339920 hasConceptScore W2807339920C77928131 @default.
• W2807339920 hasLocation W28073399201 @default.
• W2807339920 hasOpenAccess W2807339920 @default.
• W2807339920 hasPrimaryLocation W28073399201 @default.
• W2807339920 hasRelatedWork W2054247755 @default.
• W2807339920 hasRelatedWork W2054974175 @default.
• W2807339920 hasRelatedWork W2055807945 @default.
• W2807339920 hasRelatedWork W2071367639 @default.
• W2807339920 hasRelatedWork W2145168577 @default.
• W2807339920 hasRelatedWork W2163776574 @default.
• W2807339920 hasRelatedWork W2166813588 @default.
• W2807339920 hasRelatedWork W2248700751 @default.
• W2807339920 hasRelatedWork W2616231814 @default.
• W2807339920 hasRelatedWork W2738312288 @default.
• W2807339920 hasRelatedWork W2742695888 @default.
• W2807339920 hasRelatedWork W2742885591 @default.
• W2807339920 hasRelatedWork W2743246520 @default.
• W2807339920 hasRelatedWork W2744952861 @default.
• W2807339920 hasRelatedWork W2750070187 @default.
• W2807339920 hasRelatedWork W2753524609 @default.
• W2807339920 hasRelatedWork W2892306776 @default.
• W2807339920 hasRelatedWork W2969830941 @default.
• W2807339920 hasRelatedWork W403330639 @default.
• W2807339920 hasRelatedWork W2187483648 @default.
• W2807339920 isParatext "false" @default.
• W2807339920 isRetracted "false" @default.
• W2807339920 magId "2807339920" @default.
• W2807339920 workType "article" @default.