FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2086109656> ?p ?o ?g. }

• W2086109656 endingPage "222" @default.
• W2086109656 startingPage "209" @default.
• W2086109656 abstract "New δ18O and δD data confirm and amplify the conclusion by Holk et al. (1991) that, during the late Cretaceous or earliest Tertiary, there was large-scale infiltration of metamorphic water at depths of at least 15 km into the lower plate of the EPRMZ, a major crustal shear zone that transects a 15 x 15 km tonalite pluton west of Borrego Springs, California. Whole-rock δ18O values in undeformed tonalite are +11.2 ± 0.4 (n = 9) and in mylonitized tonalite are +12.3 ± 0.3 (n = 21), indicating a 1 per mil increase in 18O during open-system water-rock exchange. Quartz, feldspar, and biotite δ18O values in undeformed tonalite are +12.9 ± 0.4 (n = 8), +11.0 ± 0.6 (n = 8), and +7.7 ± 0.7 (n = 8), compared with +13.5 ± 0.2 (n = 8), +11.8 ± 0.3 (n = 9), and +9.2 ± 0.3 (n = 10) in mylonitized tonalite. The extremely uniform quartz-feldspar and quartz-biotite 18O fractionations in the mylonitized tonalite indicate equilibration at 500-600°C. Biotite and hornblende δD values from undeformed tonalite are -73 ± 3 (n = 12), compared with -52 to -68 (n = 21) in mylonitic tonalite, even though the biotite and hornblende have the same Fe/Mg (≈1.25; Anderson, 1983) in both kinds of tonalite. This implies that the EPRMZ was infiltrated by large amounts of high-D water (δD ≈ -10 to -30) at 500-600°C, probably derived at depth by dehydration of subducted oceanic crust or underplated volcanogenic sediments. Syndeformational tonalitic pegmatites have quartz and feldspar δ18O values of +13.5 ± 0.3 (n = 4) and +12.2 ± 0.3 (n = 6), and biotite and muscovite δD values of -64 ± 1 (n = 2) and -42 (n = 1), suggesting a genetic relationship between the pegmatites and these deep-seated fluids. Higher whole-rock δ18O values (+13.2 to +16.1, n = 3) and much lower δD values (-72 to -114, n = 3) occur where the EPRMZ cuts upper-plate amphibolite-facies metasediments. The shift to lower δD values in these finer grained rocks probably occurred during interactions with heated meteoric groundwaters during Pliocene detachment faulting associated with the opening of the Gulf of California." @default.
• W2086109656 created "2016-06-24" @default.
• W2086109656 creator A5000430371 @default.
• W2086109656 creator A5008638188 @default.
• W2086109656 creator A5078447569 @default.
• W2086109656 date "2006-03-01" @default.
• W2086109656 modified "2023-09-27" @default.
• W2086109656 title "Stable Isotope Evidence for Large-Scale Infiltration of Metamorphic Fluids Generated during Shallow Subduction into the Eastern Peninsular Ranges Mylonite Zone (EPRMZ), Southern California" @default.
• W2086109656 cites W1973013015 @default.
• W2086109656 cites W1976352716 @default.
• W2086109656 cites W1990057085 @default.
• W2086109656 cites W1996361224 @default.
• W2086109656 cites W2004993774 @default.
• W2086109656 cites W2008638099 @default.
• W2086109656 cites W2008937734 @default.
• W2086109656 cites W2026335482 @default.
• W2086109656 cites W2029491511 @default.
• W2086109656 cites W2034641752 @default.
• W2086109656 cites W2034727040 @default.
• W2086109656 cites W2034906094 @default.
• W2086109656 cites W2036050458 @default.
• W2086109656 cites W2045503897 @default.
• W2086109656 cites W2048912820 @default.
• W2086109656 cites W2061286155 @default.
• W2086109656 cites W2065435935 @default.
• W2086109656 cites W2067509041 @default.
• W2086109656 cites W2069243531 @default.
• W2086109656 cites W2073505354 @default.
• W2086109656 cites W2086163800 @default.
• W2086109656 cites W2090757504 @default.
• W2086109656 cites W2091934772 @default.
• W2086109656 cites W2093989613 @default.
• W2086109656 cites W2094196330 @default.
• W2086109656 cites W2094414093 @default.
• W2086109656 cites W2098813827 @default.
• W2086109656 cites W2111660215 @default.
• W2086109656 cites W2112180231 @default.
• W2086109656 cites W2121628908 @default.
• W2086109656 cites W2143045284 @default.
• W2086109656 cites W2160980032 @default.
• W2086109656 cites W2166165142 @default.
• W2086109656 cites W2323358117 @default.
• W2086109656 cites W2345932527 @default.
• W2086109656 cites W2412698757 @default.
• W2086109656 cites W2477339804 @default.
• W2086109656 cites W2588793367 @default.
• W2086109656 cites W2901876326 @default.
• W2086109656 doi "https://doi.org/10.2747/0020-6814.48.3.209" @default.
• W2086109656 hasPublicationYear "2006" @default.
• W2086109656 type Work @default.
• W2086109656 sameAs 2086109656 @default.
• W2086109656 citedByCount "5" @default.
• W2086109656 countsByYear W20861096562016 @default.
• W2086109656 countsByYear W20861096562017 @default.
• W2086109656 countsByYear W20861096562021 @default.
• W2086109656 crossrefType "journal-article" @default.
• W2086109656 hasAuthorship W2086109656A5000430371 @default.
• W2086109656 hasAuthorship W2086109656A5008638188 @default.
• W2086109656 hasAuthorship W2086109656A5078447569 @default.
• W2086109656 hasConcept C127313418 @default.
• W2086109656 hasConcept C151730666 @default.
• W2086109656 hasConcept C165205528 @default.
• W2086109656 hasConcept C17409809 @default.
• W2086109656 hasConcept C197737763 @default.
• W2086109656 hasConcept C23295444 @default.
• W2086109656 hasConcept C26687426 @default.
• W2086109656 hasConcept C2777212541 @default.
• W2086109656 hasConcept C2777229588 @default.
• W2086109656 hasConcept C2779870107 @default.
• W2086109656 hasConcept C34122518 @default.
• W2086109656 hasConcept C5900021 @default.
• W2086109656 hasConcept C77928131 @default.
• W2086109656 hasConceptScore W2086109656C127313418 @default.
• W2086109656 hasConceptScore W2086109656C151730666 @default.
• W2086109656 hasConceptScore W2086109656C165205528 @default.
• W2086109656 hasConceptScore W2086109656C17409809 @default.
• W2086109656 hasConceptScore W2086109656C197737763 @default.
• W2086109656 hasConceptScore W2086109656C23295444 @default.
• W2086109656 hasConceptScore W2086109656C26687426 @default.
• W2086109656 hasConceptScore W2086109656C2777212541 @default.
• W2086109656 hasConceptScore W2086109656C2777229588 @default.
• W2086109656 hasConceptScore W2086109656C2779870107 @default.
• W2086109656 hasConceptScore W2086109656C34122518 @default.
• W2086109656 hasConceptScore W2086109656C5900021 @default.
• W2086109656 hasConceptScore W2086109656C77928131 @default.
• W2086109656 hasIssue "3" @default.
• W2086109656 hasLocation W20861096561 @default.
• W2086109656 hasOpenAccess W2086109656 @default.
• W2086109656 hasPrimaryLocation W20861096561 @default.
• W2086109656 hasRelatedWork W152003370 @default.
• W2086109656 hasRelatedWork W2005603140 @default.
• W2086109656 hasRelatedWork W2018662544 @default.
• W2086109656 hasRelatedWork W2025055894 @default.
• W2086109656 hasRelatedWork W2025208485 @default.
• W2086109656 hasRelatedWork W2089657444 @default.
• W2086109656 hasRelatedWork W2211662185 @default.
• W2086109656 hasRelatedWork W2335456839 @default.
• W2086109656 hasRelatedWork W2384863749 @default.

• next