FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4379052007> ?p ?o ?g. }

• W4379052007 abstract "Abstract Western Tethys sedimentary successions constitute fundamental archives of Late Triassic–Early Jurassic environmental, carbonate production and tectonic changes. During the Late Triassic, the Northern Calcareous Alps (Austria) belonged to the Western Tethys passive margin, characterised by the deposition of the early-dolomitized peritidal Hauptdolomit (Norian) adjacent basinward to the Dachstein carbonate shelf and passing upward to the mixed carbonate–siliciclastic Kössen Formation (Upper Norian–Rhaetian). The Kössen Fm. was subdivided into the lower shallow-water Hochalm Member and the upper Eiberg Member, accumulated in an intraplatform basin coeval to shallow-water carbonates (Upper Rhaetian Limestone). The Eiberg Mb. and overlying Jurassic strata were extensively studied as a continuous marine record across the Triassic/Jurassic boundary. In contrast, shallow-water successions, time-equivalent to the Eiberg Mb. and Upper Rhaetian Limestone, located North of the Eiberg Basin, are poorly investigated. This study focusses on the approximately 350 m thick Norian to Lower Jurassic succession cropping out in the eastern Northern Calcareous Alps (Stumpfmauer). The 32 distinguished lithofacies compose seven, vertically superimposed, sedimentary units (A–G), belonging to the Hochalm Mb. of the Kössen Fm. (Unit A peritidal cyclothems, Unit B claystone/marlstone with fossiliferous beds, Unit C coral boundstone to floatstone), Upper Rhaetian Limestone (Unit D subtidal cyclothems with claystone), shallow-water carbonate strata transitional to Lower Jurassic (Unit E ooidal coated grain peloidal grainstone with basal transgressive lag, Unit F bivalve-rich, microbialite and oncoidal lithofacies, previously attributed to the Upper Rhaetian Limestone) and Hettangian–Sinemurian Kalksburg Fm. (Unit G cross-laminated coated grain peloidal grainstone with quartz and chert). The detailed lithofacies characterisation presented in this study contributes to the knowledge on the Northern Calcareous Alps stratigraphy and depositional environments across the Triassic/Jurassic boundary. The identified sedimentary units can be framed in the evolution of Western Tethys and share similarities with depositional systems from the Western Carpathians, Transdanubian Range, Southern Alps and Dinarides suggesting coherent sedimentary response and environmental, climate and tectonic controls in different palaeogeographic domains." @default.
• W4379052007 created "2023-06-02" @default.
• W4379052007 creator A5040957818 @default.
• W4379052007 creator A5052837329 @default.
• W4379052007 creator A5065338672 @default.
• W4379052007 date "2023-06-01" @default.
• W4379052007 modified "2023-09-26" @default.
• W4379052007 title "Facies character and evolution of a mixed carbonate–siliciclastic shelf: Upper Triassic–Lower Jurassic succession in the eastern Northern Calcareous Alps (Stumpfmauer, Austria)" @default.
• W4379052007 cites W1055786285 @default.
• W4379052007 cites W117473350 @default.
• W4379052007 cites W14176565 @default.
• W4379052007 cites W1492179824 @default.
• W4379052007 cites W1595304541 @default.
• W4379052007 cites W1966929024 @default.
• W4379052007 cites W1970674741 @default.
• W4379052007 cites W1970729026 @default.
• W4379052007 cites W1971870574 @default.
• W4379052007 cites W1974817692 @default.
• W4379052007 cites W1979676116 @default.
• W4379052007 cites W1981285400 @default.
• W4379052007 cites W1992096365 @default.
• W4379052007 cites W1994124986 @default.
• W4379052007 cites W1997469183 @default.
• W4379052007 cites W2006766138 @default.
• W4379052007 cites W2008268722 @default.
• W4379052007 cites W2009894789 @default.
• W4379052007 cites W2010219714 @default.
• W4379052007 cites W2011168485 @default.
• W4379052007 cites W2011346321 @default.
• W4379052007 cites W2021403729 @default.
• W4379052007 cites W2022609833 @default.
• W4379052007 cites W2024202801 @default.
• W4379052007 cites W2027540032 @default.
• W4379052007 cites W2033131144 @default.
• W4379052007 cites W2040535069 @default.
• W4379052007 cites W2047527622 @default.
• W4379052007 cites W2048459684 @default.
• W4379052007 cites W2048893847 @default.
• W4379052007 cites W2053385554 @default.
• W4379052007 cites W2054562150 @default.
• W4379052007 cites W2055826656 @default.
• W4379052007 cites W2059923107 @default.
• W4379052007 cites W2067067936 @default.
• W4379052007 cites W2069719632 @default.
• W4379052007 cites W2074853666 @default.
• W4379052007 cites W2077869040 @default.
• W4379052007 cites W2078388543 @default.
• W4379052007 cites W2078590009 @default.
• W4379052007 cites W2080263483 @default.
• W4379052007 cites W2081790539 @default.
• W4379052007 cites W2088197346 @default.
• W4379052007 cites W2093794784 @default.
• W4379052007 cites W2106758756 @default.
• W4379052007 cites W2111661152 @default.
• W4379052007 cites W2121834312 @default.
• W4379052007 cites W2124452066 @default.
• W4379052007 cites W2128721289 @default.
• W4379052007 cites W2139089333 @default.
• W4379052007 cites W2140594577 @default.
• W4379052007 cites W2148919921 @default.
• W4379052007 cites W2156645194 @default.
• W4379052007 cites W216821235 @default.
• W4379052007 cites W2205127574 @default.
• W4379052007 cites W2262165475 @default.
• W4379052007 cites W2281444302 @default.
• W4379052007 cites W2313844312 @default.
• W4379052007 cites W2315436207 @default.
• W4379052007 cites W2316659968 @default.
• W4379052007 cites W2316751213 @default.
• W4379052007 cites W2316800547 @default.
• W4379052007 cites W2331303754 @default.
• W4379052007 cites W2416926419 @default.
• W4379052007 cites W2544588336 @default.
• W4379052007 cites W2556480611 @default.
• W4379052007 cites W2756635838 @default.
• W4379052007 cites W2768538599 @default.
• W4379052007 cites W2783753929 @default.
• W4379052007 cites W2800504634 @default.
• W4379052007 cites W2887843553 @default.
• W4379052007 cites W2921803195 @default.
• W4379052007 cites W2963806330 @default.
• W4379052007 cites W2968591245 @default.
• W4379052007 cites W3022506140 @default.
• W4379052007 cites W3041830245 @default.
• W4379052007 cites W3047625509 @default.
• W4379052007 cites W3214367185 @default.
• W4379052007 cites W36763570 @default.
• W4379052007 cites W4230666600 @default.
• W4379052007 cites W4234446984 @default.
• W4379052007 cites W2052175445 @default.
• W4379052007 doi "https://doi.org/10.1007/s10347-023-00662-x" @default.
• W4379052007 hasPublicationYear "2023" @default.
• W4379052007 type Work @default.
• W4379052007 citedByCount "0" @default.
• W4379052007 crossrefType "journal-article" @default.
• W4379052007 hasAuthorship W4379052007A5040957818 @default.
• W4379052007 hasAuthorship W4379052007A5052837329 @default.
• W4379052007 hasAuthorship W4379052007A5065338672 @default.
• W4379052007 hasBestOaLocation W43790520071 @default.
• W4379052007 hasConcept C104873425 @default.

• next