FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2595927249> ?p ?o ?g. }

• W2595927249 endingPage "22" @default.
• W2595927249 startingPage "8" @default.
• W2595927249 abstract "The Western Falkland Islands are characterized by landforms and sediments of Quaternary age originating from the interplay of periglacial and marine processes. These have left their imprints on siliciclastic sediments and subbituminous coal, peatland, and podzolic soil. Our depositional study focuses on interpreting a stratigraphic sequence which contains white quartz sand with an interbedded coal seam by using petrography (coal petrography, carbon isotope analysis, sedimentary petrography, clay mineralogy, granulometric, morphometric studies), and geochemistry. The study of the coal-sand couple sheds some light on two contrasting sedimentary geological settings. Firstly, it broadens the knowledge of the regional geology at the southern tip of South America by examining how coal seams may be emplaced in a periglacial-microtidal environment. Secondly, the study is also relevant for applied geology by investigating how sand is processed in a coal-bearing paralic regime. The coal-sand couple evolved during 6 discrete stages. Stage I: The detrital parent material was derived from the Siluro-Carboniferous Gran Malvina Group. Stage II: From the Oligocene through the late Miocene under a warm tropical climate organic matter was accumulated in a paralic environment giving rise to subbituminous coal. Stage III: During the Pleistocene alternating erosion and deposition in a wave-dominated coastal-marine regime gave rise to the build-up of coal interbedded with sand. The hydrodynamic regime reduced the grain size to the level of medium to fine sand and enhanced its sorting coefficient causing the separation of minerals according to their specific gravity (mechanical processing). Stage IV: The coal seam has been reworked by the last glacial progradation. Stage V: Weathering by wind and waterworn sand grains into semispherical to spherical forms and the content of heavy minerals increased along backshore and in dune belt environments. Stage VI: Organic acids derived from the coal promoted chemical leaching and significantly contributed to the decrease of the labile constituents of arenites (feldspar, carbonate minerals, and calcareous tests of faunal remains). Chemical alteration was grinded to a halt by another sea level rise, which gradually destroyed the coal layer. The depositional environment most effective for the processing of sand is located in the microtidal setting. In the meso- to macrotidal hydrodynamic regime the chemical leaching becomes the only efficacious tool to improve the quality of the footwall rocks. Due to the predominance of argillaceous sediments there, the quality of clay is enhanced and kaolin deposits may come into existence." @default.
• W2595927249 created "2017-03-23" @default.
• W2595927249 creator A5014655086 @default.
• W2595927249 creator A5032006649 @default.
• W2595927249 creator A5040127049 @default.
• W2595927249 creator A5049499459 @default.
• W2595927249 creator A5070670553 @default.
• W2595927249 date "2017-04-01" @default.
• W2595927249 modified "2023-09-29" @default.
• W2595927249 title "Oligo-Miocene coal in a microtidal environment reworked under Quaternary periglacial conditions (Western Falkland Islands/Isla Gran Malvina) – Coal formation and natural sand processing" @default.
• W2595927249 cites W1534265788 @default.
• W2595927249 cites W1966354379 @default.
• W2595927249 cites W1971821852 @default.
• W2595927249 cites W1982783119 @default.
• W2595927249 cites W1984373363 @default.
• W2595927249 cites W2004132697 @default.
• W2595927249 cites W2004144637 @default.
• W2595927249 cites W2008874249 @default.
• W2595927249 cites W2020389818 @default.
• W2595927249 cites W2028630457 @default.
• W2595927249 cites W2032987328 @default.
• W2595927249 cites W2037350614 @default.
• W2595927249 cites W2037610157 @default.
• W2595927249 cites W2043890424 @default.
• W2595927249 cites W2059933723 @default.
• W2595927249 cites W2067069910 @default.
• W2595927249 cites W2080830021 @default.
• W2595927249 cites W2092309739 @default.
• W2595927249 cites W2094581504 @default.
• W2595927249 cites W2097612521 @default.
• W2595927249 cites W2129229924 @default.
• W2595927249 cites W2132656327 @default.
• W2595927249 cites W2139096962 @default.
• W2595927249 cites W2140554737 @default.
• W2595927249 cites W2154821814 @default.
• W2595927249 cites W2169463254 @default.
• W2595927249 cites W2196949306 @default.
• W2595927249 cites W2324451174 @default.
• W2595927249 cites W2503154566 @default.
• W2595927249 cites W2513287867 @default.
• W2595927249 cites W2947166117 @default.
• W2595927249 cites W3126017275 @default.
• W2595927249 cites W4236372120 @default.
• W2595927249 cites W4245476400 @default.
• W2595927249 doi "https://doi.org/10.1016/j.coal.2017.03.006" @default.
• W2595927249 hasPublicationYear "2017" @default.
• W2595927249 type Work @default.
• W2595927249 sameAs 2595927249 @default.
• W2595927249 citedByCount "6" @default.
• W2595927249 countsByYear W25959272492020 @default.
• W2595927249 countsByYear W25959272492021 @default.
• W2595927249 countsByYear W25959272492022 @default.
• W2595927249 countsByYear W25959272492023 @default.
• W2595927249 crossrefType "journal-article" @default.
• W2595927249 hasAuthorship W2595927249A5014655086 @default.
• W2595927249 hasAuthorship W2595927249A5032006649 @default.
• W2595927249 hasAuthorship W2595927249A5040127049 @default.
• W2595927249 hasAuthorship W2595927249A5049499459 @default.
• W2595927249 hasAuthorship W2595927249A5070670553 @default.
• W2595927249 hasBestOaLocation W25959272491 @default.
• W2595927249 hasConcept C109007969 @default.
• W2595927249 hasConcept C126753816 @default.
• W2595927249 hasConcept C127313418 @default.
• W2595927249 hasConcept C151730666 @default.
• W2595927249 hasConcept C166957645 @default.
• W2595927249 hasConcept C17409809 @default.
• W2595927249 hasConcept C2777031316 @default.
• W2595927249 hasConcept C518851703 @default.
• W2595927249 hasConcept C59235061 @default.
• W2595927249 hasConcept C6494504 @default.
• W2595927249 hasConcept C95457728 @default.
• W2595927249 hasConceptScore W2595927249C109007969 @default.
• W2595927249 hasConceptScore W2595927249C126753816 @default.
• W2595927249 hasConceptScore W2595927249C127313418 @default.
• W2595927249 hasConceptScore W2595927249C151730666 @default.
• W2595927249 hasConceptScore W2595927249C166957645 @default.
• W2595927249 hasConceptScore W2595927249C17409809 @default.
• W2595927249 hasConceptScore W2595927249C2777031316 @default.
• W2595927249 hasConceptScore W2595927249C518851703 @default.
• W2595927249 hasConceptScore W2595927249C59235061 @default.
• W2595927249 hasConceptScore W2595927249C6494504 @default.
• W2595927249 hasConceptScore W2595927249C95457728 @default.
• W2595927249 hasLocation W25959272491 @default.
• W2595927249 hasOpenAccess W2595927249 @default.
• W2595927249 hasPrimaryLocation W25959272491 @default.
• W2595927249 hasRelatedWork W1561775770 @default.
• W2595927249 hasRelatedWork W1969096839 @default.
• W2595927249 hasRelatedWork W2025585437 @default.
• W2595927249 hasRelatedWork W2062327081 @default.
• W2595927249 hasRelatedWork W2082235444 @default.
• W2595927249 hasRelatedWork W2089025968 @default.
• W2595927249 hasRelatedWork W2379284781 @default.
• W2595927249 hasRelatedWork W2728540815 @default.
• W2595927249 hasRelatedWork W4242351863 @default.
• W2595927249 hasRelatedWork W4253709286 @default.
• W2595927249 hasVolume "174" @default.
• W2595927249 isParatext "false" @default.
• W2595927249 isRetracted "false" @default.

• next