FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2163513149> ?p ?o ?g. }

• W2163513149 endingPage "15" @default.
• W2163513149 startingPage "1" @default.
• W2163513149 abstract "The source of Recent turbidites in the deep basins of the Marmara Sea was investigated by comparing their heavy-mineral composition with those from the beach sands of the Marmara Sea. The Marmara Sea is an inland sea between the Mediterranean and Black seas. It consists essentially of three strike–slip basins, over 1000 m deep, which are forming along the North Anatolian Fault. The thickness of the Pliocene to Recent syn-transform sediments in the Marmara basins exceeds several kilometers. Sand samples were studied at 49 locations along the Marmara Sea beaches and in 15 samples from seven cores from the basins. Based on the amount and type of heavy minerals, four heavy-mineral provinces are distinguished in the beach sands. Beach sands from the northwestern Marmara Sea are characterized by a scarcity of the heavy minerals, which are represented mainly by mica and chlorite. They are derived from erosion of the soft and friable Miocene sandstones exposed in the region. In the north-central Marmara Sea, the beach sands have a relatively high proportion of heavy minerals, which are dominated by opaques, epidote, and garnet. The heavy-mineral composition of these beach sands reflects those of the Oligocene sandstones in the hinterland. Beach sands in the eastern Marmara Sea are varied in their heavy-mineral composition, reflecting a heterogeneous hinterland. Beach sands in the southern Marmara Sea are characterized by a high proportion of heavy minerals dominated by amphibole+pyroxene, epidote, and opaque. Heavy minerals in the sandy layers in the gravity cores differ from those of the beach sands by a decrease in the concentration of high-density heavy minerals, and increase in mica and chlorite, related to transport processes. Nevertheless, comparison of the heavy-mineral assemblages and heavy-mineral ratios between the beach sands, and sands from the deep basins suggests a sediment transport from the west from the Miocene sandstones for the Western (Tekirdağ) basin. For the Central basin, sandy layers from a single gravity core show variable heavy-mineral assemblages, suggesting derivation from both north and south of the Marmara Sea. The Eastern (Çınarcık) basin receives at least some of its sandy sediment from the east through the Bay of Izmit." @default.
• W2163513149 created "2016-06-24" @default.
• W2163513149 creator A5011572860 @default.
• W2163513149 creator A5027944480 @default.
• W2163513149 date "2005-03-01" @default.
• W2163513149 modified "2023-09-25" @default.
• W2163513149 title "Source of the basinal sediments in the Marmara Sea investigated using heavy minerals in the modern beach sands" @default.
• W2163513149 cites W1869757691 @default.
• W2163513149 cites W1967675882 @default.
• W2163513149 cites W1969628787 @default.
• W2163513149 cites W1973865613 @default.
• W2163513149 cites W1975144494 @default.
• W2163513149 cites W1976715182 @default.
• W2163513149 cites W1976980525 @default.
• W2163513149 cites W1988163840 @default.
• W2163513149 cites W2004314359 @default.
• W2163513149 cites W2006110853 @default.
• W2163513149 cites W2015859409 @default.
• W2163513149 cites W2024136445 @default.
• W2163513149 cites W2041732462 @default.
• W2163513149 cites W2068109226 @default.
• W2163513149 cites W2070741293 @default.
• W2163513149 cites W2080423790 @default.
• W2163513149 cites W2084551236 @default.
• W2163513149 cites W2085580711 @default.
• W2163513149 cites W2107682097 @default.
• W2163513149 cites W2123700104 @default.
• W2163513149 cites W2162230971 @default.
• W2163513149 cites W2164821252 @default.
• W2163513149 cites W2324451174 @default.
• W2163513149 doi "https://doi.org/10.1016/j.margeo.2005.01.006" @default.
• W2163513149 hasPublicationYear "2005" @default.
• W2163513149 type Work @default.
• W2163513149 sameAs 2163513149 @default.
• W2163513149 citedByCount "33" @default.
• W2163513149 countsByYear W21635131492012 @default.
• W2163513149 countsByYear W21635131492013 @default.
• W2163513149 countsByYear W21635131492014 @default.
• W2163513149 countsByYear W21635131492015 @default.
• W2163513149 countsByYear W21635131492016 @default.
• W2163513149 countsByYear W21635131492017 @default.
• W2163513149 countsByYear W21635131492018 @default.
• W2163513149 countsByYear W21635131492019 @default.
• W2163513149 countsByYear W21635131492020 @default.
• W2163513149 countsByYear W21635131492021 @default.
• W2163513149 countsByYear W21635131492022 @default.
• W2163513149 crossrefType "journal-article" @default.
• W2163513149 hasAuthorship W2163513149A5011572860 @default.
• W2163513149 hasAuthorship W2163513149A5027944480 @default.
• W2163513149 hasConcept C127313418 @default.
• W2163513149 hasConcept C151730666 @default.
• W2163513149 hasConcept C17409809 @default.
• W2163513149 hasConcept C2777844515 @default.
• W2163513149 hasConcept C2778357522 @default.
• W2163513149 hasConcept C2779870107 @default.
• W2163513149 hasConcept C2780049196 @default.
• W2163513149 hasConcept C2781394513 @default.
• W2163513149 hasConcept C6494504 @default.
• W2163513149 hasConceptScore W2163513149C127313418 @default.
• W2163513149 hasConceptScore W2163513149C151730666 @default.
• W2163513149 hasConceptScore W2163513149C17409809 @default.
• W2163513149 hasConceptScore W2163513149C2777844515 @default.
• W2163513149 hasConceptScore W2163513149C2778357522 @default.
• W2163513149 hasConceptScore W2163513149C2779870107 @default.
• W2163513149 hasConceptScore W2163513149C2780049196 @default.
• W2163513149 hasConceptScore W2163513149C2781394513 @default.
• W2163513149 hasConceptScore W2163513149C6494504 @default.
• W2163513149 hasIssue "1-2" @default.
• W2163513149 hasLocation W21635131491 @default.
• W2163513149 hasOpenAccess W2163513149 @default.
• W2163513149 hasPrimaryLocation W21635131491 @default.
• W2163513149 hasRelatedWork W1965114414 @default.
• W2163513149 hasRelatedWork W2058559863 @default.
• W2163513149 hasRelatedWork W2329998470 @default.
• W2163513149 hasRelatedWork W2366394843 @default.
• W2163513149 hasRelatedWork W2370679613 @default.
• W2163513149 hasRelatedWork W2375244954 @default.
• W2163513149 hasRelatedWork W2376790792 @default.
• W2163513149 hasRelatedWork W2382162834 @default.
• W2163513149 hasRelatedWork W4233341916 @default.
• W2163513149 hasRelatedWork W2800734410 @default.
• W2163513149 hasVolume "216" @default.
• W2163513149 isParatext "false" @default.
• W2163513149 isRetracted "false" @default.
• W2163513149 magId "2163513149" @default.
• W2163513149 workType "article" @default.