FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2129224407> ?p ?o ?g. }

• W2129224407 endingPage "647" @default.
• W2129224407 startingPage "641" @default.
• W2129224407 abstract "An oxygen isotope study has been carried out on rocks and minerals from the 3 units which comprise the concentric Hercynian pluton of Ploumanac9h (Brittany, France). Lack of extensive low-temperature water/rock interactions enabled 3 non-cogenetic pulses of magma to be identified: (1) an early mantle-derived basaltic magma of alkaline affinity (δ 18 O ∼ 6); (2) biotite granites (δ 18 O ∼ 9) which form the bulk of the intrusion; and (3) a ring dyke of late, two mica-cordierite granite (δ 18 O = 12.3) that is clearly of crustal derivation. The δ 18 O data, together with published 87 Sr/ 86 Sr results, suggest that the last 2 (granitic) pulses were generated in the continental crust. These results are not compatible with any models of closed-system fractional crystallization of a single parent magma-type, although they probably can be fitted into a 9mixing9 model involving combined assimilation/fractional crystallization of continental crustal material by basaltic magma. A more likely explanation of the biotite granites is melting of amphibolites or granulites of the lower crust (possibly derived from volcano-detrital parent rocks), with the two-mica granites forming by melting of shallower, more pelitic metasedimentary rocks. The position of the Ploumanac9h pluton in a linear arrangement of related intrusions, together with the clear-cut structural control of its emplacement, are compatible with a model of melting at different levels in the crust and upper mantle, either associated with a mantle plume, or by a pressure release near the tip of a propagating lithospheric crack." @default.
• W2129224407 created "2016-06-24" @default.
• W2129224407 creator A5010609473 @default.
• W2129224407 creator A5054821774 @default.
• W2129224407 creator A5078447569 @default.
• W2129224407 date "1980-09-01" @default.
• W2129224407 modified "2023-10-13" @default.
• W2129224407 title "¹⁸ O/ ¹⁶ O evidence for non-cogenetic magmas associated in a 300 Ma old concentric pluton at Ploumanac'h (Brittany, France)" @default.
• W2129224407 cites W1968858830 @default.
• W2129224407 cites W1971632964 @default.
• W2129224407 cites W1971762124 @default.
• W2129224407 cites W1978318884 @default.
• W2129224407 cites W1983714152 @default.
• W2129224407 cites W1995215894 @default.
• W2129224407 cites W2008638099 @default.
• W2129224407 cites W2054408437 @default.
• W2129224407 cites W2061609249 @default.
• W2129224407 cites W2064890366 @default.
• W2129224407 cites W2078752746 @default.
• W2129224407 cites W2082068225 @default.
• W2129224407 cites W2083688044 @default.
• W2129224407 cites W2099199436 @default.
• W2129224407 cites W2168882659 @default.
• W2129224407 cites W2313877506 @default.
• W2129224407 cites W2323358117 @default.
• W2129224407 cites W2330645702 @default.
• W2129224407 cites W2334022626 @default.
• W2129224407 cites W2357876281 @default.
• W2129224407 cites W2773194484 @default.
• W2129224407 doi "https://doi.org/10.1144/gsjgs.137.5.0641" @default.
• W2129224407 hasPublicationYear "1980" @default.
• W2129224407 type Work @default.
• W2129224407 sameAs 2129224407 @default.
• W2129224407 citedByCount "13" @default.
• W2129224407 countsByYear W21292244072017 @default.
• W2129224407 countsByYear W21292244072021 @default.
• W2129224407 crossrefType "journal-article" @default.
• W2129224407 hasAuthorship W2129224407A5010609473 @default.
• W2129224407 hasAuthorship W2129224407A5054821774 @default.
• W2129224407 hasAuthorship W2129224407A5078447569 @default.
• W2129224407 hasConcept C127313418 @default.
• W2129224407 hasConcept C151730666 @default.
• W2129224407 hasConcept C17409809 @default.
• W2129224407 hasConcept C199289684 @default.
• W2129224407 hasConcept C34122518 @default.
• W2129224407 hasConcept C42787717 @default.
• W2129224407 hasConcept C77928131 @default.
• W2129224407 hasConceptScore W2129224407C127313418 @default.
• W2129224407 hasConceptScore W2129224407C151730666 @default.
• W2129224407 hasConceptScore W2129224407C17409809 @default.
• W2129224407 hasConceptScore W2129224407C199289684 @default.
• W2129224407 hasConceptScore W2129224407C34122518 @default.
• W2129224407 hasConceptScore W2129224407C42787717 @default.
• W2129224407 hasConceptScore W2129224407C77928131 @default.
• W2129224407 hasIssue "5" @default.
• W2129224407 hasLocation W21292244071 @default.
• W2129224407 hasOpenAccess W2129224407 @default.
• W2129224407 hasPrimaryLocation W21292244071 @default.
• W2129224407 hasRelatedWork W1991294353 @default.
• W2129224407 hasRelatedWork W2003761134 @default.
• W2129224407 hasRelatedWork W2042078286 @default.
• W2129224407 hasRelatedWork W2046739381 @default.
• W2129224407 hasRelatedWork W2145552873 @default.
• W2129224407 hasRelatedWork W2266498847 @default.
• W2129224407 hasRelatedWork W2361053869 @default.
• W2129224407 hasRelatedWork W2371415235 @default.
• W2129224407 hasRelatedWork W2382915239 @default.
• W2129224407 hasRelatedWork W2388994666 @default.
• W2129224407 hasVolume "137" @default.
• W2129224407 isParatext "false" @default.
• W2129224407 isRetracted "false" @default.
• W2129224407 magId "2129224407" @default.
• W2129224407 workType "article" @default.