FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1970115911> ?p ?o ?g. }

• W1970115911 endingPage "248" @default.
• W1970115911 startingPage "231" @default.
• W1970115911 abstract "The Eucla Basin has the largest onshore extent of Cenozoic marine sediments anywhere in the world. The sediments provide a record of the evolving marine environments of the Southern Ocean and the terrestrial hinterland of the Australian continent. However, owing to its size and remoteness, the Eucla Basin is comparatively understudied. This is exacerbated by the scattered and often deeply weathered nature of the outcrops along the margins of the basin, and the inaccessibility of exposures in the basin centre, except in cliffs and caves. The extent and isolation of the Eucla Basin over two states has resulted in conflicting and overlapping stratigraphic nomenclature, especially of the marginal sediments. Therefore, we propose rationalising the nomenclature of the Eocene rocks in the region based on three guiding principles: the use of consistent terminology across the region; the recognition of the importance of allostratigraphy in defining stratigraphic architecture, in particular two 3rd‐order cycles correlated with the Tortachilla and Tuketja transgressions; and continuity with past usage wherever possible, with a minimum of new terminology. We propose eight major changes to the existing nomenclature: (i) abandoning the term Bremer Basin for the marine and marginal marine to non‐marine Eocene sediments that infill palaeovalleys and form a veneer across crystalline basement in southwest Western Australia and including these sediments in the margin of the Eucla Basin; a similar situation exists in the east, where the Eocene sediments that have been included in the Polda Basin are likewise a marginal extension of the Eucla Basin; (ii) introducing the term Maralinga Formation for all Middle Eocene non‐marine to marginal marine sediments, including those previously included in the lower part of the Pidinga Formation in South Australia, and North Royal Formation for similar sediments in Western Australia; these replace the previous informal usage of lower Pidinga and lower Werillup Formation, respectively; (iii) restricting Hampton Sandstone to its original usage for a calcareous marine sand underlying the Wilson Bluff Limestone; (iv) raising the Paling Member of the Wilson Bluff Limestone to formation status; (v) using Pidinga Formation for all Upper Eocene carbonaceous sediments on the margins of the Eucla Basin in South Australia, and Werillup Formation for all such sediments in Western Australia, including the marginal palaeovalleys; terms such as Wollubar Sandstone in the palaeovalleys of the Yilgarn Craton, and Poelpena and Wanilla Formations in the Eocene part of the former Polda Basin should be abandoned; (vi) using the term Pallinup Formation for all Upper Eocene spicule‐rich sediments along the western margin of the Eucla Basin; (vii) recognising the formation status of the Upper Eocene spicular marine sediments in the eastern Eucla Basin that were formerly termed the Khasta Member of the Hampton Sandstone and the Bring Member of the Pidinga Formation, abandoning the term Bring Member, and including those rocks, and similar sediments of the Poelpena Formation in the Polda Basin, in the new Khasta Formation; and (viii) abandoning the term Toolinna Limestone previously applied to Upper Eocene grainstone along the western margin of the Eucla Basin as it is a facies of the Wilson Bluff Limestone, whereas the grainstone at the type locality at Toolinna Cove is in fact Abrakurrie Limestone and is indistinguishable from the rest of that formation. We believe this rationalisation emphasises the unity of stratigraphy across much of southern Australia and, thus, will facilitate research on the Eucla Basin as a whole." @default.
• W1970115911 created "2016-06-24" @default.
• W1970115911 creator A5005947295 @default.
• W1970115911 creator A5032647668 @default.
• W1970115911 creator A5041944618 @default.
• W1970115911 creator A5042392339 @default.
• W1970115911 date "2003-04-01" @default.
• W1970115911 modified "2023-09-24" @default.
• W1970115911 title "Middle to Upper Eocene stratigraphic nomenclature and deposition in the Eucla Basin" @default.
• W1970115911 cites W1548360498 @default.
• W1970115911 cites W1971411049 @default.
• W1970115911 cites W1980413582 @default.
• W1970115911 cites W2004114920 @default.
• W1970115911 cites W2009580673 @default.
• W1970115911 cites W2015218318 @default.
• W1970115911 cites W2016003832 @default.
• W1970115911 cites W2017548112 @default.
• W1970115911 cites W2027068856 @default.
• W1970115911 cites W2027145314 @default.
• W1970115911 cites W2027420308 @default.
• W1970115911 cites W2034716029 @default.
• W1970115911 cites W2049966744 @default.
• W1970115911 cites W2056015374 @default.
• W1970115911 cites W2067575761 @default.
• W1970115911 cites W2078507095 @default.
• W1970115911 cites W2096051666 @default.
• W1970115911 cites W2116850928 @default.
• W1970115911 cites W2123635152 @default.
• W1970115911 cites W2124774832 @default.
• W1970115911 cites W2130950244 @default.
• W1970115911 cites W2150279650 @default.
• W1970115911 cites W2477629636 @default.
• W1970115911 cites W2482312745 @default.
• W1970115911 cites W2687631996 @default.
• W1970115911 cites W2734431908 @default.
• W1970115911 cites W2749338807 @default.
• W1970115911 cites W2991444189 @default.
• W1970115911 cites W3008688422 @default.
• W1970115911 cites W3118431851 @default.
• W1970115911 cites W586462836 @default.
• W1970115911 cites W639794298 @default.
• W1970115911 cites W757020703 @default.
• W1970115911 doi "https://doi.org/10.1046/j.1440-0952.2003.00995.x" @default.
• W1970115911 hasPublicationYear "2003" @default.
• W1970115911 type Work @default.
• W1970115911 sameAs 1970115911 @default.
• W1970115911 citedByCount "41" @default.
• W1970115911 countsByYear W19701159112013 @default.
• W1970115911 countsByYear W19701159112014 @default.
• W1970115911 countsByYear W19701159112016 @default.
• W1970115911 countsByYear W19701159112017 @default.
• W1970115911 countsByYear W19701159112018 @default.
• W1970115911 countsByYear W19701159112019 @default.
• W1970115911 countsByYear W19701159112020 @default.
• W1970115911 countsByYear W19701159112021 @default.
• W1970115911 countsByYear W19701159112022 @default.
• W1970115911 countsByYear W19701159112023 @default.
• W1970115911 crossrefType "journal-article" @default.
• W1970115911 hasAuthorship W1970115911A5005947295 @default.
• W1970115911 hasAuthorship W1970115911A5032647668 @default.
• W1970115911 hasAuthorship W1970115911A5041944618 @default.
• W1970115911 hasAuthorship W1970115911A5042392339 @default.
• W1970115911 hasConcept C109007969 @default.
• W1970115911 hasConcept C127313418 @default.
• W1970115911 hasConcept C146588470 @default.
• W1970115911 hasConcept C151730666 @default.
• W1970115911 hasConcept C166957645 @default.
• W1970115911 hasConcept C169212394 @default.
• W1970115911 hasConcept C205649164 @default.
• W1970115911 hasConcept C2776340010 @default.
• W1970115911 hasConcept C2781297371 @default.
• W1970115911 hasConcept C73707237 @default.
• W1970115911 hasConceptScore W1970115911C109007969 @default.
• W1970115911 hasConceptScore W1970115911C127313418 @default.
• W1970115911 hasConceptScore W1970115911C146588470 @default.
• W1970115911 hasConceptScore W1970115911C151730666 @default.
• W1970115911 hasConceptScore W1970115911C166957645 @default.
• W1970115911 hasConceptScore W1970115911C169212394 @default.
• W1970115911 hasConceptScore W1970115911C205649164 @default.
• W1970115911 hasConceptScore W1970115911C2776340010 @default.
• W1970115911 hasConceptScore W1970115911C2781297371 @default.
• W1970115911 hasConceptScore W1970115911C73707237 @default.
• W1970115911 hasIssue "2" @default.
• W1970115911 hasLocation W19701159111 @default.
• W1970115911 hasOpenAccess W1970115911 @default.
• W1970115911 hasPrimaryLocation W19701159111 @default.
• W1970115911 hasRelatedWork W1978330345 @default.
• W1970115911 hasRelatedWork W2003500372 @default.
• W1970115911 hasRelatedWork W2023045059 @default.
• W1970115911 hasRelatedWork W2126640245 @default.
• W1970115911 hasRelatedWork W2169779506 @default.
• W1970115911 hasRelatedWork W2318626169 @default.
• W1970115911 hasRelatedWork W2368224014 @default.
• W1970115911 hasRelatedWork W2370445142 @default.
• W1970115911 hasRelatedWork W2374445754 @default.
• W1970115911 hasRelatedWork W2995812845 @default.
• W1970115911 hasVolume "50" @default.
• W1970115911 isParatext "false" @default.

• next