FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2073669747> ?p ?o ?g. }

• W2073669747 endingPage "313" @default.
• W2073669747 startingPage "303" @default.
• W2073669747 abstract "Abstract A magnetic polarity reversal near the top of the Tumblagooda Sandstone, in the Carnarvon Basin, Western Australia, has been intensively investigated in five coastal sections and four inland sections, all located near the top of the formation. A further four inland sections towards the base of the formation were also sampled. Of the inland sections, all but two are suspected to have been largely remagnetized in similar fashion to Late Palaeozoic and Mesozoic sediments to the south. At the remaining seven sections a zone of normal magnetization overlies a zone of mixed (coexisting normal and reversed) magnetization, and the boundary between them coincides with a unique marker horizon of pebbly sandstone. The intimate relationship of the (virtual) reversal and the pebble marker horizon lends strong support to the suggestion that erosional stripping accompanied the formation of the pebble marker. The pebble marker is best interpreted as a lag deposit. The stratigraphic coincidence does not necessarily signify the concurrence of a reversal with the formation of the marker horizon, but rather that the relationship represents a variation on the unconformity test. The record of the actual geomagnetic reversal has been physically removed from most sections. These results show conclusively that the age of the magnetization of the Tumblagooda Sandstone is very close to the age of deposition, and can therefore provide an important pole for the definition of the Gondwana apparent polar wander path. However, the suggested Silurian age must be questioned on the basis of the palaeomagnetism which best accords with an Ordovician age. The lower parts of the sequence may be as old as the Cambrian. While the age of the palaeomagnetic pole from the Tumblagooda Sandstone is therefore not well constrained, its position is well defined and in combination with other Gondwana poles indicates a period of rapid polar motion during the Ordovician/Silurian. A collision with Laurasia at the end of the Silurian and beginning of the Devonian may explain the timing of the Caledonian/Acadian Orogenies." @default.
• W2073669747 created "2016-06-24" @default.
• W2073669747 creator A5008103628 @default.
• W2073669747 creator A5089349816 @default.
• W2073669747 date "1990-12-01" @default.
• W2073669747 modified "2023-10-14" @default.
• W2073669747 title "The palaeomagnetism of the Tumblagooda Sandstone, Western Australia: Gondwana palaeozoic apparent polar wandering" @default.
• W2073669747 cites W1971450949 @default.
• W2073669747 cites W1978485464 @default.
• W2073669747 cites W1982477790 @default.
• W2073669747 cites W2011283441 @default.
• W2073669747 cites W2034029151 @default.
• W2073669747 cites W2040414906 @default.
• W2073669747 cites W2045716692 @default.
• W2073669747 cites W2050434458 @default.
• W2073669747 cites W2055997967 @default.
• W2073669747 cites W2063258367 @default.
• W2073669747 cites W2085435956 @default.
• W2073669747 cites W2095845960 @default.
• W2073669747 cites W2111740379 @default.
• W2073669747 cites W2117805437 @default.
• W2073669747 cites W2145488282 @default.
• W2073669747 cites W2149255556 @default.
• W2073669747 cites W2152289537 @default.
• W2073669747 cites W2152327304 @default.
• W2073669747 cites W2164736653 @default.
• W2073669747 cites W2165542051 @default.
• W2073669747 cites W2300688371 @default.
• W2073669747 doi "https://doi.org/10.1016/0031-9201(90)90045-y" @default.
• W2073669747 hasPublicationYear "1990" @default.
• W2073669747 type Work @default.
• W2073669747 sameAs 2073669747 @default.
• W2073669747 citedByCount "12" @default.
• W2073669747 countsByYear W20736697472012 @default.
• W2073669747 countsByYear W20736697472016 @default.
• W2073669747 countsByYear W20736697472017 @default.
• W2073669747 countsByYear W20736697472018 @default.
• W2073669747 countsByYear W20736697472021 @default.
• W2073669747 crossrefType "journal-article" @default.
• W2073669747 hasAuthorship W2073669747A5008103628 @default.
• W2073669747 hasAuthorship W2073669747A5089349816 @default.
• W2073669747 hasConcept C114749048 @default.
• W2073669747 hasConcept C121332964 @default.
• W2073669747 hasConcept C127313418 @default.
• W2073669747 hasConcept C1276947 @default.
• W2073669747 hasConcept C13106087 @default.
• W2073669747 hasConcept C151730666 @default.
• W2073669747 hasConcept C189479680 @default.
• W2073669747 hasConcept C2781121502 @default.
• W2073669747 hasConcept C2781148125 @default.
• W2073669747 hasConcept C29705727 @default.
• W2073669747 hasConcept C77928131 @default.
• W2073669747 hasConceptScore W2073669747C114749048 @default.
• W2073669747 hasConceptScore W2073669747C121332964 @default.
• W2073669747 hasConceptScore W2073669747C127313418 @default.
• W2073669747 hasConceptScore W2073669747C1276947 @default.
• W2073669747 hasConceptScore W2073669747C13106087 @default.
• W2073669747 hasConceptScore W2073669747C151730666 @default.
• W2073669747 hasConceptScore W2073669747C189479680 @default.
• W2073669747 hasConceptScore W2073669747C2781121502 @default.
• W2073669747 hasConceptScore W2073669747C2781148125 @default.
• W2073669747 hasConceptScore W2073669747C29705727 @default.
• W2073669747 hasConceptScore W2073669747C77928131 @default.
• W2073669747 hasIssue "2-4" @default.
• W2073669747 hasLocation W20736697471 @default.
• W2073669747 hasOpenAccess W2073669747 @default.
• W2073669747 hasPrimaryLocation W20736697471 @default.
• W2073669747 hasRelatedWork W1979530313 @default.
• W2073669747 hasRelatedWork W1993867113 @default.
• W2073669747 hasRelatedWork W2008947219 @default.
• W2073669747 hasRelatedWork W2009900653 @default.
• W2073669747 hasRelatedWork W2030407912 @default.
• W2073669747 hasRelatedWork W2072819303 @default.
• W2073669747 hasRelatedWork W2152327304 @default.
• W2073669747 hasRelatedWork W2167094019 @default.
• W2073669747 hasRelatedWork W2363421968 @default.
• W2073669747 hasRelatedWork W4251503598 @default.
• W2073669747 hasVolume "64" @default.
• W2073669747 isParatext "false" @default.
• W2073669747 isRetracted "false" @default.
• W2073669747 magId "2073669747" @default.
• W2073669747 workType "article" @default.