FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2062562104> ?p ?o ?g. }

• W2062562104 endingPage "292" @default.
• W2062562104 startingPage "281" @default.
• W2062562104 abstract "The geology of Mahé-Island and adjoining islets, Seychelles, consists of three types of late Precambrian granitic rock series: (1) a gneissose granodiorite-gneissose tonalite and amphibolite-leucogranodiorite series, (2) a porphyritic granite-pink granite series, and (3) a grey granite-gneissose grey granite series. All these granitic rocks are cut by dykes of doleritic compositions, mostly with a WNW-ESE trend. The gneissose granodiorite is a calcalkaline I-type granite with normative Ab ⪢ Or, the porphyritic granite is a sub-alkaline A-type granite with normative Ab > Or, and the grey granite is an alkaline A-type granite with normative Ab > Or. RbSr radiometric analyses yielded ages of 713±19 Ma for the gneissose granodiorite, 683±16 Ma for the porphyritic granite and 570±5 Ma for the grey granite. Petrological, geological, geochronological and geochemical studies suggest that the late Precambrian granitic rocks of the Seychelles are very similar to, and are well correlated with those of the Arabian-Nubian shield. 408 late Precambrian granite specimens were collected from the Mahé island group, Seychelles. Progressive alternating field demagnetization and thermal demagnetization have been successfully performed to isolate stable remanence with well-grouped direction from natural remanent magnetization of the granites. The stable remanences of the granite fall around a northerly mean direction, of which the declination is 348.5° and the inclination +48.7°. The stable remanences of the Mahé island group granite yield a palaeomagnetic pole at 54.0°N, 38.2°E. From the above data, in conjunction with reported polar wander path and plate rotation poles, it is concluded that the Seychelles were originally located near the eastern end of the Horn of Africa and have drifted to the present position since continental break-up." @default.
• W2062562104 created "2016-06-24" @default.
• W2062562104 creator A5010714226 @default.
• W2062562104 creator A5052528842 @default.
• W2062562104 creator A5074192078 @default.
• W2062562104 date "1994-10-01" @default.
• W2062562104 modified "2023-09-28" @default.
• W2062562104 title "Palaeomagnetic and petrological reconstruction of the Seychelles" @default.
• W2062562104 cites W1967038717 @default.
• W2062562104 cites W1978676610 @default.
• W2062562104 cites W1993715318 @default.
• W2062562104 cites W2000021617 @default.
• W2062562104 cites W2007470916 @default.
• W2062562104 cites W2013487351 @default.
• W2062562104 cites W2017184974 @default.
• W2062562104 cites W2021423539 @default.
• W2062562104 cites W2035114293 @default.
• W2062562104 cites W2038371312 @default.
• W2062562104 cites W2041379989 @default.
• W2062562104 cites W2050186146 @default.
• W2062562104 cites W2062310854 @default.
• W2062562104 cites W2092629490 @default.
• W2062562104 cites W2108971421 @default.
• W2062562104 cites W2112931403 @default.
• W2062562104 cites W2318543838 @default.
• W2062562104 cites W4249152216 @default.
• W2062562104 doi "https://doi.org/10.1016/0301-9268(94)90092-2" @default.
• W2062562104 hasPublicationYear "1994" @default.
• W2062562104 type Work @default.
• W2062562104 sameAs 2062562104 @default.
• W2062562104 citedByCount "23" @default.
• W2062562104 countsByYear W20625621042012 @default.
• W2062562104 countsByYear W20625621042013 @default.
• W2062562104 countsByYear W20625621042014 @default.
• W2062562104 countsByYear W20625621042017 @default.
• W2062562104 countsByYear W20625621042018 @default.
• W2062562104 countsByYear W20625621042019 @default.
• W2062562104 countsByYear W20625621042020 @default.
• W2062562104 crossrefType "journal-article" @default.
• W2062562104 hasAuthorship W2062562104A5010714226 @default.
• W2062562104 hasAuthorship W2062562104A5052528842 @default.
• W2062562104 hasAuthorship W2062562104A5074192078 @default.
• W2062562104 hasConcept C127313418 @default.
• W2062562104 hasConcept C151730666 @default.
• W2062562104 hasConcept C170187044 @default.
• W2062562104 hasConcept C173776410 @default.
• W2062562104 hasConcept C17409809 @default.
• W2062562104 hasConcept C2779670319 @default.
• W2062562104 hasConcept C2779870107 @default.
• W2062562104 hasConceptScore W2062562104C127313418 @default.
• W2062562104 hasConceptScore W2062562104C151730666 @default.
• W2062562104 hasConceptScore W2062562104C170187044 @default.
• W2062562104 hasConceptScore W2062562104C173776410 @default.
• W2062562104 hasConceptScore W2062562104C17409809 @default.
• W2062562104 hasConceptScore W2062562104C2779670319 @default.
• W2062562104 hasConceptScore W2062562104C2779870107 @default.
• W2062562104 hasIssue "1-4" @default.
• W2062562104 hasLocation W20625621041 @default.
• W2062562104 hasOpenAccess W2062562104 @default.
• W2062562104 hasPrimaryLocation W20625621041 @default.
• W2062562104 hasRelatedWork W1528554604 @default.
• W2062562104 hasRelatedWork W1987691177 @default.
• W2062562104 hasRelatedWork W2022575623 @default.
• W2062562104 hasRelatedWork W2062562104 @default.
• W2062562104 hasRelatedWork W2325748159 @default.
• W2062562104 hasRelatedWork W2349947565 @default.
• W2062562104 hasRelatedWork W2357710212 @default.
• W2062562104 hasRelatedWork W2528248850 @default.
• W2062562104 hasRelatedWork W3172595358 @default.
• W2062562104 hasRelatedWork W2578123099 @default.
• W2062562104 hasVolume "69" @default.
• W2062562104 isParatext "false" @default.
• W2062562104 isRetracted "false" @default.
• W2062562104 magId "2062562104" @default.
• W2062562104 workType "article" @default.