FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000075387> ?p ?o ?g. }

• W2000075387 endingPage "157" @default.
• W2000075387 startingPage "135" @default.
• W2000075387 abstract "The Žacléř coalfield in the western part of the Intra-Sudetic Basin is an example of coal accumulation in an alluvial valley deposited under a long-term (~ 3 m.y.) stable tectonic regime, with climatic oscillations possibly operating on several time scales. The resulting sedimentary record, about 600 m thick, encompasses about 60 coal-bearing cycles formed in a relatively small and localized part of the valley, whereas elsewhere a higher clastic input and/or lower rate of subsidence resulted in deposition of strata with very little coal. Available data suggest that tectonics produced accommodation for sediments and, via changes in topography and/or size of the source area, affected the volume and dispersal patterns of clastic material transported to the depocentre. Areas with long-term tectonic stability were suitable places for recognition of climatic signals in the sedimentary record, modified by the intensity of local clastic input. Climatic fluctuations generated coal-bearing cycles, probably through a variable intensity of precipitation which affected the density of vegetation cover across the landscape along with evaporation and groundwater table. These factors influenced the intensity of chemical weathering and hence regulated the volume and composition of clastics delivered to the depocentre. This in turn resulted in alternation of short periods of bedload-dominated deposition during the seasonally dry part of the cycle with periods of dominantly suspended load and organic (peat) deposition during the more humid (?everwet) part of the cycle. Estimated duration of the basic cycles (~ 46 k.y.) approximates the orbitally-driven axial tilt cyclicity. Basic cycles are arranged into two larger-scale cyclic patterns lasting for 270 k.y. and 1.5 m.y., respectively, which broadly correspond with the timing of glacial maxima and minima inferred from high-latitude glacial deposits of Gondwanan basins. All the coals of the Žacléř coalfield display similar petrographic composition dominated by collotelinite, and field observations as well as detailed petrographic study show that they formed in planar rheotrophic peat swamps where long-lasting peat accretion was episodically interrupted only by major floods on a century to millennial scale." @default.
• W2000075387 created "2016-06-24" @default.
• W2000075387 creator A5004252776 @default.
• W2000075387 creator A5022374641 @default.
• W2000075387 creator A5066827229 @default.
• W2000075387 date "2013-09-01" @default.
• W2000075387 modified "2023-10-18" @default.
• W2000075387 title "Climatic vs. tectonic controls on peat accretion in non-marine setting; an example from the Žacléř Formation (Yeadonian–Bolsovian) in the Intra-Sudetic Basin (Czech Republic)" @default.
• W2000075387 cites W1789049081 @default.
• W2000075387 cites W1964641312 @default.
• W2000075387 cites W1966550075 @default.
• W2000075387 cites W1977069895 @default.
• W2000075387 cites W1979392144 @default.
• W2000075387 cites W1984703252 @default.
• W2000075387 cites W1992879104 @default.
• W2000075387 cites W1999206191 @default.
• W2000075387 cites W2001813295 @default.
• W2000075387 cites W2005013588 @default.
• W2000075387 cites W2005291615 @default.
• W2000075387 cites W2009179398 @default.
• W2000075387 cites W2013414780 @default.
• W2000075387 cites W2020928880 @default.
• W2000075387 cites W2027480374 @default.
• W2000075387 cites W2028097183 @default.
• W2000075387 cites W2041788078 @default.
• W2000075387 cites W2042347616 @default.
• W2000075387 cites W2042594107 @default.
• W2000075387 cites W2043243253 @default.
• W2000075387 cites W2043399946 @default.
• W2000075387 cites W2044042101 @default.
• W2000075387 cites W2047174461 @default.
• W2000075387 cites W2048109598 @default.
• W2000075387 cites W2048378779 @default.
• W2000075387 cites W2051534897 @default.
• W2000075387 cites W2056138418 @default.
• W2000075387 cites W2058795006 @default.
• W2000075387 cites W2060173587 @default.
• W2000075387 cites W2061319664 @default.
• W2000075387 cites W2063252704 @default.
• W2000075387 cites W2069792062 @default.
• W2000075387 cites W2073986814 @default.
• W2000075387 cites W2074297072 @default.
• W2000075387 cites W2074328626 @default.
• W2000075387 cites W2076261307 @default.
• W2000075387 cites W2081296107 @default.
• W2000075387 cites W2094701466 @default.
• W2000075387 cites W2122759092 @default.
• W2000075387 cites W2122810456 @default.
• W2000075387 cites W2122949014 @default.
• W2000075387 cites W2123919668 @default.
• W2000075387 cites W2129090345 @default.
• W2000075387 cites W2129454037 @default.
• W2000075387 cites W2131272880 @default.
• W2000075387 cites W2133417869 @default.
• W2000075387 cites W2148975479 @default.
• W2000075387 cites W2154930938 @default.
• W2000075387 cites W2156484412 @default.
• W2000075387 cites W2156939454 @default.
• W2000075387 cites W2318217881 @default.
• W2000075387 cites W3126017275 @default.
• W2000075387 cites W4211110706 @default.
• W2000075387 cites W4253952146 @default.
• W2000075387 doi "https://doi.org/10.1016/j.coal.2013.07.011" @default.
• W2000075387 hasPublicationYear "2013" @default.
• W2000075387 type Work @default.
• W2000075387 sameAs 2000075387 @default.
• W2000075387 citedByCount "33" @default.
• W2000075387 countsByYear W20000753872013 @default.
• W2000075387 countsByYear W20000753872014 @default.
• W2000075387 countsByYear W20000753872015 @default.
• W2000075387 countsByYear W20000753872016 @default.
• W2000075387 countsByYear W20000753872017 @default.
• W2000075387 countsByYear W20000753872018 @default.
• W2000075387 countsByYear W20000753872019 @default.
• W2000075387 countsByYear W20000753872020 @default.
• W2000075387 countsByYear W20000753872021 @default.
• W2000075387 countsByYear W20000753872022 @default.
• W2000075387 countsByYear W20000753872023 @default.
• W2000075387 crossrefType "journal-article" @default.
• W2000075387 hasAuthorship W2000075387A5004252776 @default.
• W2000075387 hasAuthorship W2000075387A5022374641 @default.
• W2000075387 hasAuthorship W2000075387A5066827229 @default.
• W2000075387 hasConcept C109007969 @default.
• W2000075387 hasConcept C114793014 @default.
• W2000075387 hasConcept C126753816 @default.
• W2000075387 hasConcept C127313418 @default.
• W2000075387 hasConcept C138170599 @default.
• W2000075387 hasConcept C151730666 @default.
• W2000075387 hasConcept C17409809 @default.
• W2000075387 hasConcept C18903297 @default.
• W2000075387 hasConcept C193748577 @default.
• W2000075387 hasConcept C53657456 @default.
• W2000075387 hasConcept C64297162 @default.
• W2000075387 hasConcept C6494504 @default.
• W2000075387 hasConcept C77928131 @default.
• W2000075387 hasConcept C86803240 @default.
• W2000075387 hasConceptScore W2000075387C109007969 @default.
• W2000075387 hasConceptScore W2000075387C114793014 @default.

• next