FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2110069564> ?p ?o ?g. }

• W2110069564 endingPage "262" @default.
• W2110069564 startingPage "256" @default.
• W2110069564 abstract "Abstract Coarse-grained strata deposited on continental shelves and epeiric seas in some tens of meters' water depth are conventionally ascribed simply to storms of varying intensity which interrupted the settling out of suspended mud. Surprisingly, the possibility of tsunamis is virtually never evaluated even though they might, indeed should, have been common in many regions. Portions of the Middle Cambrian La Laja Formation of the Argentine Precordillera formed in such a submerged epeiric platform or shelf. They comprise a suite of three limestone facies: variably argillaceous burrowed mudstone, bioclastic grainstone, and intraclastic conglomerate composed of pieces of mudstone including cemented haloes around burrows. Sporadically developed eocrinoid meadows and trilobite populations are recorded respectively by disarticulated ossicles and usually broken sclerites. The latter indicate that, generally, exoskeletons became fragmented by repeated bottom turbulence. Hence, the mudstones and grainstones show that, before stabilization by calcite cementation which began beneath the sediment–water interface and away from burrow margins, physical reworking of the surface sediment by storms was so frequent that it did not leave a specific signature of individual events. By contrast, scattered lenticular beds of intraclastic conglomerate were due to anomalous, brief episodes of deep scour and strong oscillatory flow from powerful wave action. These conglomerates then escaped subsequent reworking. Because they are abruptly interbedded and encased within uniform mudstone, and there are no stratigraphic patterns, allochthonous material, or unconformities to indicate sea-level fluctuation, the events that created the conglomerates were more likely tsunamis, not storms. They could have been unleashed by faulting elsewhere on the shelf or rifting beyond the shelf margin to the (present-day) west to southwest. Those originating in the rift basin may have been diffracted by marginal shoals and attenuated by the shallowness of the platform which caused the waves to break some distance offshore. In any case, the study area was not affected by backwash. Recognition of tsunami-laid beds urges a reexamination of the standard tempestite paradigm with its use of coarse-grained strata as a simple measure of storm frequency and intensity." @default.
• W2110069564 created "2016-06-24" @default.
• W2110069564 creator A5066944658 @default.
• W2110069564 creator A5081853275 @default.
• W2110069564 date "2007-04-01" @default.
• W2110069564 modified "2023-10-17" @default.
• W2110069564 title "Tsunamis in a Stormy Sea: Middle Cambrian Inner-Shelf Limestones of Western Argentina" @default.
• W2110069564 cites W1646260529 @default.
• W2110069564 cites W1832705977 @default.
• W2110069564 cites W1882725046 @default.
• W2110069564 cites W1938697528 @default.
• W2110069564 cites W1972862743 @default.
• W2110069564 cites W1980516075 @default.
• W2110069564 cites W1988040128 @default.
• W2110069564 cites W1995071771 @default.
• W2110069564 cites W2007266279 @default.
• W2110069564 cites W2008169371 @default.
• W2110069564 cites W2027633350 @default.
• W2110069564 cites W2029268904 @default.
• W2110069564 cites W2031584075 @default.
• W2110069564 cites W2047253135 @default.
• W2110069564 cites W2059063101 @default.
• W2110069564 cites W2065093349 @default.
• W2110069564 cites W2074562907 @default.
• W2110069564 cites W2083076018 @default.
• W2110069564 cites W2086275488 @default.
• W2110069564 cites W2092555112 @default.
• W2110069564 cites W2095809405 @default.
• W2110069564 cites W2099800603 @default.
• W2110069564 cites W2111478699 @default.
• W2110069564 cites W2124772045 @default.
• W2110069564 cites W2134109299 @default.
• W2110069564 cites W2135766579 @default.
• W2110069564 cites W2147066104 @default.
• W2110069564 cites W2152842730 @default.
• W2110069564 cites W2160919684 @default.
• W2110069564 cites W2164842700 @default.
• W2110069564 cites W2165841751 @default.
• W2110069564 cites W284770056 @default.
• W2110069564 cites W2988762248 @default.
• W2110069564 doi "https://doi.org/10.2110/jsr.2007.032" @default.
• W2110069564 hasPublicationYear "2007" @default.
• W2110069564 type Work @default.
• W2110069564 sameAs 2110069564 @default.
• W2110069564 citedByCount "43" @default.
• W2110069564 countsByYear W21100695642012 @default.
• W2110069564 countsByYear W21100695642013 @default.
• W2110069564 countsByYear W21100695642014 @default.
• W2110069564 countsByYear W21100695642015 @default.
• W2110069564 countsByYear W21100695642016 @default.
• W2110069564 countsByYear W21100695642018 @default.
• W2110069564 countsByYear W21100695642019 @default.
• W2110069564 countsByYear W21100695642020 @default.
• W2110069564 countsByYear W21100695642021 @default.
• W2110069564 countsByYear W21100695642022 @default.
• W2110069564 countsByYear W21100695642023 @default.
• W2110069564 crossrefType "journal-article" @default.
• W2110069564 hasAuthorship W2110069564A5066944658 @default.
• W2110069564 hasAuthorship W2110069564A5081853275 @default.
• W2110069564 hasConcept C111368507 @default.
• W2110069564 hasConcept C127313418 @default.
• W2110069564 hasConcept C151730666 @default.
• W2110069564 hasConceptScore W2110069564C111368507 @default.
• W2110069564 hasConceptScore W2110069564C127313418 @default.
• W2110069564 hasConceptScore W2110069564C151730666 @default.
• W2110069564 hasIssue "4" @default.
• W2110069564 hasLocation W21100695641 @default.
• W2110069564 hasOpenAccess W2110069564 @default.
• W2110069564 hasPrimaryLocation W21100695641 @default.
• W2110069564 hasRelatedWork W1606027898 @default.
• W2110069564 hasRelatedWork W1995827510 @default.
• W2110069564 hasRelatedWork W2038586383 @default.
• W2110069564 hasRelatedWork W2049667995 @default.
• W2110069564 hasRelatedWork W2059394852 @default.
• W2110069564 hasRelatedWork W2275812285 @default.
• W2110069564 hasRelatedWork W2325222095 @default.
• W2110069564 hasRelatedWork W2773498057 @default.
• W2110069564 hasRelatedWork W2789304626 @default.
• W2110069564 hasRelatedWork W2911869918 @default.
• W2110069564 hasVolume "77" @default.
• W2110069564 isParatext "false" @default.
• W2110069564 isRetracted "false" @default.
• W2110069564 magId "2110069564" @default.
• W2110069564 workType "article" @default.