FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2011056630> ?p ?o ?g. }

• W2011056630 endingPage "432" @default.
• W2011056630 startingPage "401" @default.
• W2011056630 abstract "A regional seismic synthesis of the 10 km-thick continental and shallow-marine succession of the Bowen Basin has revealed the basin-filling episodes and nine depositional supersequences (A–I). An Early Permian extensional phase, characterised by thick volcanics and half-graben development in a number of separated troughs, allowed fluviolacustrine sediments, including coal, to accumulate (Supersequence A). In the subsequent thermal subsidence phase, four marine supersequences (B–E) were generated. The onsets of supersequences B and C appear to be primarily tectonically controlled, but there is no evidence of tectonism initiating D, E and F. Supersequences B, D and E start with marine-flooding events, and in the Denison Trough end with either non-marine progradation (B), or high-energy nearshore sands (D and E). The first evidence of the compressional deformation associated with the development of a foreland basin occurs at the base of deltaic to marine Supersequence C. The thrust-induced loading of the foreland caused rapid subsidence in the adjacent Taroom Trough. It took about 10 Ma for the effects of thrust loading to spread across the basin from east to west. The foreland loading first affected the entire basin at the time of Late Permian Supersequence F, and lasted until the end of Triassic deposition. Four supersequences (F–I) have been identified in this phase of basin evolution. The later part of Supersequence F is almost wholly non-marine coal measures. The tectonism and base-level fall that generated the sequence boundary between Supersequences F and G, and ended coal deposition, represents a significant hiatus, and in places is characterised by low-angle unconformity and erosion. The pattern of the remaining units of the foreland basin phase indicates episodic basin filling as accommodation space became available, related to pulses of thrust loading. The regional geometry of the units, and the overstepping of Supersequence G by H, and then by I, indicates continuing westward progradation of foreland loading and corresponding changes in accommodation. It is striking that although the late foreland-loading phase displays the greatest rate of subsidence affecting the basin since the initial rift phase, there is little evidence of widespread flooding by the sea. The reasons were probably that the Late Permian–Early Triassic was a time of global first-order lowstand, and that foreland loading was able to provide simultaneously high rates of subsidence in the basin and greatly increased sediment supply from erosion in the mountains thrust up to the east." @default.
• W2011056630 created "2016-06-24" @default.
• W2011056630 creator A5021957932 @default.
• W2011056630 creator A5042658053 @default.
• W2011056630 creator A5062093837 @default.
• W2011056630 creator A5085427231 @default.
• W2011056630 date "2009-04-01" @default.
• W2011056630 modified "2023-10-06" @default.
• W2011056630 title "Sequence stratigraphy and fill history of the Bowen Basin, Queensland" @default.
• W2011056630 cites W1580287752 @default.
• W2011056630 cites W1584354900 @default.
• W2011056630 cites W1931933798 @default.
• W2011056630 cites W1968670931 @default.
• W2011056630 cites W1969939401 @default.
• W2011056630 cites W1972643957 @default.
• W2011056630 cites W1995438459 @default.
• W2011056630 cites W1997252211 @default.
• W2011056630 cites W1999688352 @default.
• W2011056630 cites W1999772080 @default.
• W2011056630 cites W2029580428 @default.
• W2011056630 cites W2056386844 @default.
• W2011056630 cites W2066310401 @default.
• W2011056630 cites W2068429641 @default.
• W2011056630 cites W2089856672 @default.
• W2011056630 cites W2110071674 @default.
• W2011056630 cites W2110366794 @default.
• W2011056630 cites W2318877923 @default.
• W2011056630 cites W2737379676 @default.
• W2011056630 cites W2749515094 @default.
• W2011056630 doi "https://doi.org/10.1080/08120090802698711" @default.
• W2011056630 hasPublicationYear "2009" @default.
• W2011056630 type Work @default.
• W2011056630 sameAs 2011056630 @default.
• W2011056630 citedByCount "33" @default.
• W2011056630 countsByYear W20110566302012 @default.
• W2011056630 countsByYear W20110566302015 @default.
• W2011056630 countsByYear W20110566302016 @default.
• W2011056630 countsByYear W20110566302017 @default.
• W2011056630 countsByYear W20110566302018 @default.
• W2011056630 countsByYear W20110566302020 @default.
• W2011056630 countsByYear W20110566302021 @default.
• W2011056630 countsByYear W20110566302023 @default.
• W2011056630 crossrefType "journal-article" @default.
• W2011056630 hasAuthorship W2011056630A5021957932 @default.
• W2011056630 hasAuthorship W2011056630A5042658053 @default.
• W2011056630 hasAuthorship W2011056630A5062093837 @default.
• W2011056630 hasAuthorship W2011056630A5085427231 @default.
• W2011056630 hasConcept C100951216 @default.
• W2011056630 hasConcept C109007969 @default.
• W2011056630 hasConcept C114793014 @default.
• W2011056630 hasConcept C126753816 @default.
• W2011056630 hasConcept C127313418 @default.
• W2011056630 hasConcept C139719470 @default.
• W2011056630 hasConcept C151730666 @default.
• W2011056630 hasConcept C162324750 @default.
• W2011056630 hasConcept C16565575 @default.
• W2011056630 hasConcept C17409809 @default.
• W2011056630 hasConcept C180851071 @default.
• W2011056630 hasConcept C193748577 @default.
• W2011056630 hasConcept C32239851 @default.
• W2011056630 hasConcept C6494504 @default.
• W2011056630 hasConcept C83365034 @default.
• W2011056630 hasConceptScore W2011056630C100951216 @default.
• W2011056630 hasConceptScore W2011056630C109007969 @default.
• W2011056630 hasConceptScore W2011056630C114793014 @default.
• W2011056630 hasConceptScore W2011056630C126753816 @default.
• W2011056630 hasConceptScore W2011056630C127313418 @default.
• W2011056630 hasConceptScore W2011056630C139719470 @default.
• W2011056630 hasConceptScore W2011056630C151730666 @default.
• W2011056630 hasConceptScore W2011056630C162324750 @default.
• W2011056630 hasConceptScore W2011056630C16565575 @default.
• W2011056630 hasConceptScore W2011056630C17409809 @default.
• W2011056630 hasConceptScore W2011056630C180851071 @default.
• W2011056630 hasConceptScore W2011056630C193748577 @default.
• W2011056630 hasConceptScore W2011056630C32239851 @default.
• W2011056630 hasConceptScore W2011056630C6494504 @default.
• W2011056630 hasConceptScore W2011056630C83365034 @default.
• W2011056630 hasIssue "3" @default.
• W2011056630 hasLocation W20110566301 @default.
• W2011056630 hasOpenAccess W2011056630 @default.
• W2011056630 hasPrimaryLocation W20110566301 @default.
• W2011056630 hasRelatedWork W1991816519 @default.
• W2011056630 hasRelatedWork W2030312931 @default.
• W2011056630 hasRelatedWork W2052350071 @default.
• W2011056630 hasRelatedWork W2057062325 @default.
• W2011056630 hasRelatedWork W2083156744 @default.
• W2011056630 hasRelatedWork W2090042968 @default.
• W2011056630 hasRelatedWork W2329647001 @default.
• W2011056630 hasRelatedWork W2352584650 @default.
• W2011056630 hasRelatedWork W2361296489 @default.
• W2011056630 hasRelatedWork W2361473311 @default.
• W2011056630 hasVolume "56" @default.
• W2011056630 isParatext "false" @default.
• W2011056630 isRetracted "false" @default.
• W2011056630 magId "2011056630" @default.
• W2011056630 workType "article" @default.