FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1599697801> ?p ?o ?g. }

• W1599697801 endingPage "597" @default.
• W1599697801 startingPage "557" @default.
• W1599697801 abstract "Based on lithofacies analysis of clastic, clay and carbonate rocks, wireline logs and sequence stratigraphy, sixteen depositional sequences have been distinguished in the paralic Carboniferous succession of the Lublin Basin from the Visean to the base of Westphalian B. The facies evolution and depositional architecture of the deposits belonging to three types of depositional systems tracts, i.e. lowstand (LST), transgressive (TST) and highstand (HST) have been reconstructed. The sequences are bounded by type 1 basal unconformities formed during subaerial erosion following relative sea-level fall and lowstand. This erosion, that in some cases reached down to the LST deposits of the underlying sequences, mainly affected the HST deposits. Relative sea-level rise controlling the base level of the rivers during lowstand was the basic factor influencing facies development, cyclicity and thickness of fluvial deposits, as well as the vertical and lateral transformation of rivers in the paralic Carboniferous succession. Vertical transition of high- to low-energy fluvial environments can be observed within the LST. The LST deposits typically occur in incised shelf valleys and in non-incised fluvial systems. Within the LST of sequences 2 and 4 to 10 commonly occur medium and large systems of simple incised valleys that developed in a coastal-plain system. The LST of sequences 11 to 15 comprises large systems of compound incised valleys that developed in a piedmont system. Relative sealevel rise in the late lowstand, sea-level oscillations during transgression and highstand and the volume of sediment supply were the main factors influencing facies development, cyclicity, thickness and lateral distribution of the deltaic deposits, shallow-shelf shales and limestones. Within the TST commonly occur coarsening-upward and non-gradational cyclothems that correspond to parasequences and were formed in the distal parts of the inner-shelf delta lobes. In the HST, the most common types are coarsening-upward cyclothems developed during the progradation of innershelf delta lobes and small lake deltas, as well as non-gradational cyclothems formed in lakes on a delta plain without influence of delta lobes. The transgression of sequence 7 probably had the widest extent of all the sequences in the paralic Carboniferous succession of the Lublin Basin. It was presumably much wider to the N, NE and NW than the presently accepted boundaries of the basin. Based on analysis of three curves of relative sea-level changes in the paralic Carboniferous succession of the Lublin Basin and the transgressive-regressive curve for the Carboniferous of Western Europe, the sequences distinguished have been correlated with the chronostratigraphic scheme for the Carboniferous System. The diachronous commencement of sedimentation has been confirmed and evaluated. The lack of deposits of sequence 5 in the eastern part of the basin suggests the presence of a stratigraphic gap encompassing the upper Brigantian. The position and range of stratigraphic gaps present elsewhere in the basin has also been indicated. In the north-westernmost and easternmost parts of the study area the gap has the widest range, encompassing the upper Arnsbergian to lower Marsdenian strata. The mid-Carboniferous boundary between the Mississippian and Pennsylvanian has been located at the base of sequence 8." @default.
• W1599697801 created "2016-06-24" @default.
• W1599697801 creator A5085391095 @default.
• W1599697801 date "2010-12-10" @default.
• W1599697801 modified "2023-09-26" @default.
• W1599697801 title "Sequence stratigraphy of Carboniferous paralic deposits in the Lublin Basin (SE Poland)" @default.
• W1599697801 cites W1507743074 @default.
• W1599697801 cites W1518311132 @default.
• W1599697801 cites W1519896813 @default.
• W1599697801 cites W1584140374 @default.
• W1599697801 cites W1595026935 @default.
• W1599697801 cites W1903939191 @default.
• W1599697801 cites W1912927042 @default.
• W1599697801 cites W1920329065 @default.
• W1599697801 cites W1936358913 @default.
• W1599697801 cites W1972249456 @default.
• W1599697801 cites W1980431904 @default.
• W1599697801 cites W1982829915 @default.
• W1599697801 cites W1983230959 @default.
• W1599697801 cites W1991037148 @default.
• W1599697801 cites W2003687696 @default.
• W1599697801 cites W2007721934 @default.
• W1599697801 cites W2010763757 @default.
• W1599697801 cites W2016010669 @default.
• W1599697801 cites W2018858924 @default.
• W1599697801 cites W2020700198 @default.
• W1599697801 cites W2026449169 @default.
• W1599697801 cites W2033401139 @default.
• W1599697801 cites W2039617890 @default.
• W1599697801 cites W2039890251 @default.
• W1599697801 cites W2040584918 @default.
• W1599697801 cites W2043126201 @default.
• W1599697801 cites W2043396789 @default.
• W1599697801 cites W2051650633 @default.
• W1599697801 cites W2057184487 @default.
• W1599697801 cites W2061858157 @default.
• W1599697801 cites W2063459590 @default.
• W1599697801 cites W2069792062 @default.
• W1599697801 cites W2070496895 @default.
• W1599697801 cites W2073308923 @default.
• W1599697801 cites W2095767150 @default.
• W1599697801 cites W2099581206 @default.
• W1599697801 cites W2112365365 @default.
• W1599697801 cites W2116967044 @default.
• W1599697801 cites W2118685727 @default.
• W1599697801 cites W2140709095 @default.
• W1599697801 cites W2141713510 @default.
• W1599697801 cites W2144015427 @default.
• W1599697801 cites W2147576281 @default.
• W1599697801 cites W2153901413 @default.
• W1599697801 cites W2155305561 @default.
• W1599697801 cites W2162353505 @default.
• W1599697801 cites W2163185817 @default.
• W1599697801 cites W2165291453 @default.
• W1599697801 cites W2173189143 @default.
• W1599697801 cites W2173258587 @default.
• W1599697801 cites W2175898977 @default.
• W1599697801 cites W2202312325 @default.
• W1599697801 cites W2220328515 @default.
• W1599697801 cites W2247039082 @default.
• W1599697801 cites W2254111748 @default.
• W1599697801 cites W2298208628 @default.
• W1599697801 cites W2335806871 @default.
• W1599697801 cites W2336427359 @default.
• W1599697801 cites W2344932412 @default.
• W1599697801 cites W2347127687 @default.
• W1599697801 cites W2357568415 @default.
• W1599697801 cites W2393283186 @default.
• W1599697801 cites W2505191053 @default.
• W1599697801 cites W2552418993 @default.
• W1599697801 cites W2578276576 @default.
• W1599697801 cites W2761833625 @default.
• W1599697801 cites W2035252872 @default.
• W1599697801 cites W2343286993 @default.
• W1599697801 cites W2465272552 @default.
• W1599697801 hasPublicationYear "2010" @default.
• W1599697801 type Work @default.
• W1599697801 sameAs 1599697801 @default.
• W1599697801 citedByCount "8" @default.
• W1599697801 countsByYear W15996978012012 @default.
• W1599697801 countsByYear W15996978012013 @default.
• W1599697801 countsByYear W15996978012014 @default.
• W1599697801 countsByYear W15996978012015 @default.
• W1599697801 countsByYear W15996978012016 @default.
• W1599697801 countsByYear W15996978012019 @default.
• W1599697801 countsByYear W15996978012020 @default.
• W1599697801 crossrefType "journal-article" @default.
• W1599697801 hasAuthorship W1599697801A5085391095 @default.
• W1599697801 hasConcept C109007969 @default.
• W1599697801 hasConcept C111368507 @default.
• W1599697801 hasConcept C112959462 @default.
• W1599697801 hasConcept C126753816 @default.
• W1599697801 hasConcept C127313418 @default.
• W1599697801 hasConcept C146588470 @default.
• W1599697801 hasConcept C149918038 @default.
• W1599697801 hasConcept C151730666 @default.
• W1599697801 hasConcept C191735495 @default.
• W1599697801 hasConcept C42907665 @default.

• next