FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3158581185> ?p ?o ?g. }

• W3158581185 abstract "Mesozoic ophiolites are an important feature of Cuban geology. Although Cuban ophiolites have been studied over the past 40 years, there is still need for systematic studies regarding their internal structure, geochemical characteristics, and emplacement mechanisms. The ophiolites are distributed along the so-called “Northern” and “Eastern” Cuban ophiolite belts, and are strongly dismembered and intermingled mainly with Cretaceous volcanic arc rocks. Ophiolite-associated basalts along the northern Cuban orogenic belt record magmatic history of the ophiolite formation from the Protocaribbean seafloor spreading to subduction initiation stage. We have compiled geochemical data of 15 oceanic basalt samples from previous works, together with data of an analyzed sample during this study. We discuss geochemical criteria based on immobile element proxies for fractionation indices, alkalinity, mantle flow and subduction addition, and field relationships, providing a comprehensive ophiolite classification according to the tectonic setting at which these ophiolites formed. The lavas exhibit three magmatic types. One type has subduction-related fingerprint with dominance of boninite and IAT affinities, likely related to a forearc setting. The second type has a MOR-type (N-MORB and E-MORB) signature, most of them carrying a subtle influence of subduction component, overlapping a border of the backarc field. Subordinately, a transitional type occurs with MOR-type-OIB fingerprint that is considered most likely plume-type ophiolite. The results show then that the studied lavas correspond mostly to subduction-related ophiolite and some of them have incorporated subduction component probably during the time when the Protocaribbean oceanic lithosphere downgoing beneath the Caribbean plate. Some rare remnants of plume-MORB-type ophiolite have also occurred." @default.
• W3158581185 created "2021-05-10" @default.
• W3158581185 creator A5073909615 @default.
• W3158581185 creator A5084944585 @default.
• W3158581185 date "2021-01-01" @default.
• W3158581185 modified "2023-09-26" @default.
• W3158581185 title "Geochemical Fingerprinting of Ancient Oceanic Basalts: Classification of the Cuban Ophiolites" @default.
• W3158581185 cites W1969845853 @default.
• W3158581185 cites W1978795897 @default.
• W3158581185 cites W1980220653 @default.
• W3158581185 cites W1993374359 @default.
• W3158581185 cites W1999448338 @default.
• W3158581185 cites W2010741958 @default.
• W3158581185 cites W2012834236 @default.
• W3158581185 cites W2036016724 @default.
• W3158581185 cites W2098325010 @default.
• W3158581185 cites W2105076784 @default.
• W3158581185 cites W2116044416 @default.
• W3158581185 cites W2118480431 @default.
• W3158581185 cites W2142179024 @default.
• W3158581185 cites W2312828419 @default.
• W3158581185 cites W2320437412 @default.
• W3158581185 cites W2536045657 @default.
• W3158581185 cites W2571354911 @default.
• W3158581185 doi "https://doi.org/10.1007/978-3-030-67798-5_6" @default.
• W3158581185 hasPublicationYear "2021" @default.
• W3158581185 type Work @default.
• W3158581185 sameAs 3158581185 @default.
• W3158581185 citedByCount "0" @default.
• W3158581185 crossrefType "book-chapter" @default.
• W3158581185 hasAuthorship W3158581185A5073909615 @default.
• W3158581185 hasAuthorship W3158581185A5084944585 @default.
• W3158581185 hasConcept C127313418 @default.
• W3158581185 hasConcept C151730666 @default.
• W3158581185 hasConcept C154200439 @default.
• W3158581185 hasConcept C161509811 @default.
• W3158581185 hasConcept C17409809 @default.
• W3158581185 hasConcept C192717286 @default.
• W3158581185 hasConcept C1965285 @default.
• W3158581185 hasConcept C23923706 @default.
• W3158581185 hasConcept C58097730 @default.
• W3158581185 hasConcept C77928131 @default.
• W3158581185 hasConcept C94436079 @default.
• W3158581185 hasConceptScore W3158581185C127313418 @default.
• W3158581185 hasConceptScore W3158581185C151730666 @default.
• W3158581185 hasConceptScore W3158581185C154200439 @default.
• W3158581185 hasConceptScore W3158581185C161509811 @default.
• W3158581185 hasConceptScore W3158581185C17409809 @default.
• W3158581185 hasConceptScore W3158581185C192717286 @default.
• W3158581185 hasConceptScore W3158581185C1965285 @default.
• W3158581185 hasConceptScore W3158581185C23923706 @default.
• W3158581185 hasConceptScore W3158581185C58097730 @default.
• W3158581185 hasConceptScore W3158581185C77928131 @default.
• W3158581185 hasConceptScore W3158581185C94436079 @default.
• W3158581185 hasLocation W31585811851 @default.
• W3158581185 hasOpenAccess W3158581185 @default.
• W3158581185 hasPrimaryLocation W31585811851 @default.
• W3158581185 hasRelatedWork W43882282 @default.
• W3158581185 hasRelatedWork W50857311 @default.
• W3158581185 hasRelatedWork W67655698 @default.
• W3158581185 hasRelatedWork W718504 @default.
• W3158581185 hasRelatedWork W76480875 @default.
• W3158581185 hasRelatedWork W84718659 @default.
• W3158581185 hasRelatedWork W87367526 @default.
• W3158581185 hasRelatedWork W1497674 @default.
• W3158581185 hasRelatedWork W19130679 @default.
• W3158581185 hasRelatedWork W33725190 @default.
• W3158581185 isParatext "false" @default.
• W3158581185 isRetracted "false" @default.
• W3158581185 magId "3158581185" @default.
• W3158581185 workType "book-chapter" @default.