FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2790982754> ?p ?o ?g. }

• W2790982754 endingPage "2934" @default.
• W2790982754 startingPage "2918" @default.
• W2790982754 abstract "The Cretaceous (Cenomanian, ~96 Ma) basaltic rocks of the Strand Fiord Formation of the Sverdrup Basin of the Canadian Arctic Archipelago, Nunavut, Canada, are a part of the High Arctic large igneous province. The basaltic suite reaches a thickness of almost 1,000 m on Axel Heiberg Island in its depocentre and over 700 m at the studied section. The rocks are variably fractionated tholeiitic basalts, which are geochemically similar to many other continental flood basalts, particularly to low Ti basalts of flood basalt provinces. Geochemical as well as Sr ( 87 Sr/ 86 Sr initial ~ 0.7045 to 0.7067) and Nd (Ɛ Nd(t) ~ +1.3 to +4.3) isotopic signatures of the basalts were inherited during partial melting of spinel peridotite of an ancient subcontinental lithospheric mantle, which was modified around 0.7–0.9 Ga by a metasomatic event. The melting generating the Cretaceous basalts was probably triggered by a mantle plume but was also associated with basin rifting and stretching. There is evidence of plume‐induced doming and uplift of the crust prior to and during the eruption of the basalts as documented by the progression from marine sedimentation to subaerial/lacustrine and then back to marine sedimentation in the Sverdrup Basin centre. The basalts represent parts of the Early Cretaceous igneous province that is dispersed around the Arctic Ocean due to the opening of the Canada Basin, which is inferred to be related to a mantle plume." @default.
• W2790982754 created "2018-03-29" @default.
• W2790982754 creator A5046369043 @default.
• W2790982754 creator A5084338246 @default.
• W2790982754 date "2018-01-17" @default.
• W2790982754 modified "2023-10-05" @default.
• W2790982754 title "Cretaceous basalts of the High Arctic large igneous province at Axel Heiberg Island (Canada): Volcanic stratigraphy, geodynamic setting, and origin" @default.
• W2790982754 cites W1748608781 @default.
• W2790982754 cites W1899646852 @default.
• W2790982754 cites W1921158974 @default.
• W2790982754 cites W1966917681 @default.
• W2790982754 cites W1972170017 @default.
• W2790982754 cites W1974216077 @default.
• W2790982754 cites W1979694545 @default.
• W2790982754 cites W1982431325 @default.
• W2790982754 cites W1986727686 @default.
• W2790982754 cites W1991209188 @default.
• W2790982754 cites W2001426491 @default.
• W2790982754 cites W2003034738 @default.
• W2790982754 cites W2004418855 @default.
• W2790982754 cites W2011863281 @default.
• W2790982754 cites W2012330745 @default.
• W2790982754 cites W2012760325 @default.
• W2790982754 cites W2015262698 @default.
• W2790982754 cites W2016047860 @default.
• W2790982754 cites W2018396915 @default.
• W2790982754 cites W2021754290 @default.
• W2790982754 cites W2021987309 @default.
• W2790982754 cites W2022316305 @default.
• W2790982754 cites W2022577453 @default.
• W2790982754 cites W2022648729 @default.
• W2790982754 cites W2024326960 @default.
• W2790982754 cites W2026394602 @default.
• W2790982754 cites W2045707782 @default.
• W2790982754 cites W2047064423 @default.
• W2790982754 cites W2055083480 @default.
• W2790982754 cites W2056854714 @default.
• W2790982754 cites W2060888544 @default.
• W2790982754 cites W2066735401 @default.
• W2790982754 cites W2068541972 @default.
• W2790982754 cites W2088223235 @default.
• W2790982754 cites W2091758632 @default.
• W2790982754 cites W2091828485 @default.
• W2790982754 cites W2093567690 @default.
• W2790982754 cites W2100384649 @default.
• W2790982754 cites W2102586727 @default.
• W2790982754 cites W2104769192 @default.
• W2790982754 cites W2112435406 @default.
• W2790982754 cites W2115493548 @default.
• W2790982754 cites W2117996530 @default.
• W2790982754 cites W2122213004 @default.
• W2790982754 cites W2127080669 @default.
• W2790982754 cites W2138522501 @default.
• W2790982754 cites W2139737137 @default.
• W2790982754 cites W2140496118 @default.
• W2790982754 cites W2142165173 @default.
• W2790982754 cites W2146997704 @default.
• W2790982754 cites W2148151176 @default.
• W2790982754 cites W2157099954 @default.
• W2790982754 cites W2158468162 @default.
• W2790982754 cites W2161188118 @default.
• W2790982754 cites W2170274166 @default.
• W2790982754 cites W2247207871 @default.
• W2790982754 cites W2324032452 @default.
• W2790982754 cites W2325019720 @default.
• W2790982754 cites W2462717200 @default.
• W2790982754 cites W2466821217 @default.
• W2790982754 cites W2501247117 @default.
• W2790982754 cites W2501988626 @default.
• W2790982754 cites W2910381863 @default.
• W2790982754 cites W4232396042 @default.
• W2790982754 cites W4245638129 @default.
• W2790982754 cites W4248498778 @default.
• W2790982754 doi "https://doi.org/10.1002/gj.3132" @default.
• W2790982754 hasPublicationYear "2018" @default.
• W2790982754 type Work @default.
• W2790982754 sameAs 2790982754 @default.
• W2790982754 citedByCount "15" @default.
• W2790982754 countsByYear W27909827542019 @default.
• W2790982754 countsByYear W27909827542020 @default.
• W2790982754 countsByYear W27909827542021 @default.
• W2790982754 countsByYear W27909827542023 @default.
• W2790982754 crossrefType "journal-article" @default.
• W2790982754 hasAuthorship W2790982754A5046369043 @default.
• W2790982754 hasAuthorship W2790982754A5084338246 @default.
• W2790982754 hasConcept C109007969 @default.
• W2790982754 hasConcept C127313418 @default.
• W2790982754 hasConcept C147894010 @default.
• W2790982754 hasConcept C151730666 @default.
• W2790982754 hasConcept C161509811 @default.
• W2790982754 hasConcept C162973429 @default.
• W2790982754 hasConcept C167919410 @default.
• W2790982754 hasConcept C16942324 @default.
• W2790982754 hasConcept C17409809 @default.
• W2790982754 hasConcept C2777110262 @default.
• W2790982754 hasConcept C42787717 @default.
• W2790982754 hasConcept C50682988 @default.
• W2790982754 hasConcept C6363049 @default.

• next