FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1673668717> ?p ?o ?g. }

• W1673668717 endingPage "323" @default.
• W1673668717 startingPage "308" @default.
• W1673668717 abstract "In this paper we present new paleomagnetic and paleontological data from the Ordovician and Silurian carbonate rocks of Kotelny Island (the Anjou Archipelago), and from the Ordovician turbidities of Bennett Island (the De Long Archipelago). It is assumed that both archipelagos belong to the NSI (New Siberian Islands) terrane — a key tectonic element in the Arctic region. Ages of the studied rocks have been established by paleontological data and lithological correlations. Our new data on conodonts combined with those from previous studies of Ordovician and Silurian fauna indicate a biogeographic similarity between the shelves of the Siberian paleocontinent and the NSI in the Early Paleozoic. Three new paleomagnetic poles for the NSI (48.9°N, 13.8°E, A95 = 18.1° for 475 Ma; 45.5°N, 31.9°E, A95 = 11.0° for 465 Ma, and 33.7°N, 55.7°E, A95 = 11.0° for 435 Ma) fall between the south-eastern part of Central Europe and the Zagros Mountains. The similarity of paleomagnetic directions from Kotelny and Bennet islands confirms that both the Anjou and De Long archipelagos belong to the same terrane. Calculated paleolatitudes indicate that in Ordovician–Silurian times this terrane has been located between 30° and 45°, possibly in the northern hemisphere. Based on this observation, we suggest a linkage between the NSI and the Kolyma–Omolon superterrane. Comparison of apparent polar wander paths (APWPs) of the NSI, Siberia and other cratons/terranes suggests that the NSI drifted independently. We demonstrate that the structural line between Svyatoy Nos Peninsula and Great Lyakhovsky Island is the continuation of the Kolyma Loop suture on the Arctic shelf, and expect that the continuation of the South Anyui suture is to be found east of the NSI." @default.
• W1673668717 created "2016-06-24" @default.
• W1673668717 creator A5003710186 @default.
• W1673668717 creator A5008470341 @default.
• W1673668717 creator A5027554063 @default.
• W1673668717 creator A5048463918 @default.
• W1673668717 creator A5079407706 @default.
• W1673668717 creator A5079656533 @default.
• W1673668717 date "2016-09-01" @default.
• W1673668717 modified "2023-10-16" @default.
• W1673668717 title "First paleomagnetic data for the New Siberian Islands: Implications for Arctic paleogeography" @default.
• W1673668717 cites W1966416320 @default.
• W1673668717 cites W1969760052 @default.
• W1673668717 cites W1974032983 @default.
• W1673668717 cites W1974250208 @default.
• W1673668717 cites W1975537797 @default.
• W1673668717 cites W1977317536 @default.
• W1673668717 cites W1981959946 @default.
• W1673668717 cites W1982194640 @default.
• W1673668717 cites W1995483079 @default.
• W1673668717 cites W2004918097 @default.
• W1673668717 cites W2020352059 @default.
• W1673668717 cites W2027024972 @default.
• W1673668717 cites W2028373945 @default.
• W1673668717 cites W2034067633 @default.
• W1673668717 cites W2034924757 @default.
• W1673668717 cites W2038449935 @default.
• W1673668717 cites W2041522432 @default.
• W1673668717 cites W2043260111 @default.
• W1673668717 cites W2045092811 @default.
• W1673668717 cites W2048310849 @default.
• W1673668717 cites W2060039518 @default.
• W1673668717 cites W2063011872 @default.
• W1673668717 cites W2066112144 @default.
• W1673668717 cites W2067613031 @default.
• W1673668717 cites W2069911041 @default.
• W1673668717 cites W2078112110 @default.
• W1673668717 cites W2082188140 @default.
• W1673668717 cites W2082940308 @default.
• W1673668717 cites W2083028246 @default.
• W1673668717 cites W2090286629 @default.
• W1673668717 cites W2091392627 @default.
• W1673668717 cites W2094133047 @default.
• W1673668717 cites W2095800081 @default.
• W1673668717 cites W2095815346 @default.
• W1673668717 cites W2104584561 @default.
• W1673668717 cites W2104604784 @default.
• W1673668717 cites W2109239990 @default.
• W1673668717 cites W2118204502 @default.
• W1673668717 cites W2118515467 @default.
• W1673668717 cites W2121928663 @default.
• W1673668717 cites W2128956731 @default.
• W1673668717 cites W2130601332 @default.
• W1673668717 cites W2134728822 @default.
• W1673668717 cites W2139017221 @default.
• W1673668717 cites W2145308185 @default.
• W1673668717 cites W2159592773 @default.
• W1673668717 cites W2319533243 @default.
• W1673668717 doi "https://doi.org/10.1016/j.gr.2015.08.008" @default.
• W1673668717 hasPublicationYear "2016" @default.
• W1673668717 type Work @default.
• W1673668717 sameAs 1673668717 @default.
• W1673668717 citedByCount "13" @default.
• W1673668717 countsByYear W16736687172017 @default.
• W1673668717 countsByYear W16736687172018 @default.
• W1673668717 countsByYear W16736687172020 @default.
• W1673668717 countsByYear W16736687172021 @default.
• W1673668717 countsByYear W16736687172022 @default.
• W1673668717 crossrefType "journal-article" @default.
• W1673668717 hasAuthorship W1673668717A5003710186 @default.
• W1673668717 hasAuthorship W1673668717A5008470341 @default.
• W1673668717 hasAuthorship W1673668717A5027554063 @default.
• W1673668717 hasAuthorship W1673668717A5048463918 @default.
• W1673668717 hasAuthorship W1673668717A5079407706 @default.
• W1673668717 hasAuthorship W1673668717A5079656533 @default.
• W1673668717 hasConcept C111368507 @default.
• W1673668717 hasConcept C127313418 @default.
• W1673668717 hasConcept C13106087 @default.
• W1673668717 hasConcept C147717901 @default.
• W1673668717 hasConcept C150999391 @default.
• W1673668717 hasConcept C151730666 @default.
• W1673668717 hasConcept C189479680 @default.
• W1673668717 hasConcept C204207459 @default.
• W1673668717 hasConcept C2777040169 @default.
• W1673668717 hasConcept C2779124908 @default.
• W1673668717 hasConcept C2781121502 @default.
• W1673668717 hasConcept C518008717 @default.
• W1673668717 hasConcept C77928131 @default.
• W1673668717 hasConcept C91442348 @default.
• W1673668717 hasConceptScore W1673668717C111368507 @default.
• W1673668717 hasConceptScore W1673668717C127313418 @default.
• W1673668717 hasConceptScore W1673668717C13106087 @default.
• W1673668717 hasConceptScore W1673668717C147717901 @default.
• W1673668717 hasConceptScore W1673668717C150999391 @default.
• W1673668717 hasConceptScore W1673668717C151730666 @default.
• W1673668717 hasConceptScore W1673668717C189479680 @default.
• W1673668717 hasConceptScore W1673668717C204207459 @default.
• W1673668717 hasConceptScore W1673668717C2777040169 @default.

• next