Matches in SemOpenAlex for { <https://semopenalex.org/work/W4383313391> ?p ?o ?g. }
- W4383313391 endingPage "859" @default.
- W4383313391 startingPage "855" @default.
- W4383313391 abstract "Abstract Spring waters from across the Costa Rica margin were analyzed for their Li and He isotope compositions to determine the utility of Li isotopes as a tracer of volatile sources in subduction zones. Li isotope ratios systematically decrease with increasing depth to the subducting slab: averaging +15.0‰ ± 9.2‰ in the outer forearc (<40 km to the slab), +9.3‰ ± 4.3‰ in the forearc (40–80 km to the slab), and +5.8‰ ± 2.8‰ in the arc (>80 km to the slab). In contrast, air-corrected 3He/4He values (reported relative to the ratio in air, RA) range from 0.4 to 7.5 RA and increase from predominantly crustal values near the trench to mantle values in the arc. Together, these data support progressive devolatilization of the subducting plate with slab-derived Li components sourced from shallowly expelled pore fluids in the outer forearc, sedimentary and/or altered oceanic crust contributing to the forearc, and limited slab input beneath the arc." @default.
- W4383313391 created "2023-07-07" @default.
- W4383313391 creator A5009480444 @default.
- W4383313391 creator A5020740177 @default.
- W4383313391 creator A5046994850 @default.
- W4383313391 creator A5051693546 @default.
- W4383313391 creator A5052302040 @default.
- W4383313391 creator A5060309762 @default.
- W4383313391 creator A5092242310 @default.
- W4383313391 date "2023-07-06" @default.
- W4383313391 modified "2023-09-30" @default.
- W4383313391 title "Li isotope ratios of spring fluids as an effective tracer of slab-derived subducted sources across the Costa Rica forearc" @default.
- W4383313391 cites W1495164327 @default.
- W4383313391 cites W1875122749 @default.
- W4383313391 cites W1894181983 @default.
- W4383313391 cites W1964783670 @default.
- W4383313391 cites W1966476375 @default.
- W4383313391 cites W1968394970 @default.
- W4383313391 cites W1969761050 @default.
- W4383313391 cites W1975951422 @default.
- W4383313391 cites W1976700000 @default.
- W4383313391 cites W1986603363 @default.
- W4383313391 cites W1991442438 @default.
- W4383313391 cites W2022900900 @default.
- W4383313391 cites W2035821968 @default.
- W4383313391 cites W2037389187 @default.
- W4383313391 cites W2042302826 @default.
- W4383313391 cites W2065186430 @default.
- W4383313391 cites W2072836657 @default.
- W4383313391 cites W2077578738 @default.
- W4383313391 cites W2095365910 @default.
- W4383313391 cites W2100015756 @default.
- W4383313391 cites W2105517742 @default.
- W4383313391 cites W2112213574 @default.
- W4383313391 cites W2129868779 @default.
- W4383313391 cites W2146063546 @default.
- W4383313391 cites W2148055882 @default.
- W4383313391 cites W2766342570 @default.
- W4383313391 cites W2942483658 @default.
- W4383313391 cites W2963042431 @default.
- W4383313391 cites W3047939202 @default.
- W4383313391 doi "https://doi.org/10.1130/g51277.1" @default.
- W4383313391 hasPublicationYear "2023" @default.
- W4383313391 type Work @default.
- W4383313391 citedByCount "0" @default.
- W4383313391 crossrefType "journal-article" @default.
- W4383313391 hasAuthorship W4383313391A5009480444 @default.
- W4383313391 hasAuthorship W4383313391A5020740177 @default.
- W4383313391 hasAuthorship W4383313391A5046994850 @default.
- W4383313391 hasAuthorship W4383313391A5051693546 @default.
- W4383313391 hasAuthorship W4383313391A5052302040 @default.
- W4383313391 hasAuthorship W4383313391A5060309762 @default.
- W4383313391 hasAuthorship W4383313391A5092242310 @default.
- W4383313391 hasBestOaLocation W43833133912 @default.
- W4383313391 hasConcept C113740112 @default.
- W4383313391 hasConcept C121332964 @default.
- W4383313391 hasConcept C127313418 @default.
- W4383313391 hasConcept C154200439 @default.
- W4383313391 hasConcept C155310634 @default.
- W4383313391 hasConcept C164304813 @default.
- W4383313391 hasConcept C165205528 @default.
- W4383313391 hasConcept C17409809 @default.
- W4383313391 hasConcept C178790620 @default.
- W4383313391 hasConcept C185592680 @default.
- W4383313391 hasConcept C2776698055 @default.
- W4383313391 hasConcept C2779227376 @default.
- W4383313391 hasConcept C58097730 @default.
- W4383313391 hasConcept C62520636 @default.
- W4383313391 hasConcept C67236022 @default.
- W4383313391 hasConcept C73462661 @default.
- W4383313391 hasConcept C77928131 @default.
- W4383313391 hasConcept C8058405 @default.
- W4383313391 hasConcept C94436079 @default.
- W4383313391 hasConceptScore W4383313391C113740112 @default.
- W4383313391 hasConceptScore W4383313391C121332964 @default.
- W4383313391 hasConceptScore W4383313391C127313418 @default.
- W4383313391 hasConceptScore W4383313391C154200439 @default.
- W4383313391 hasConceptScore W4383313391C155310634 @default.
- W4383313391 hasConceptScore W4383313391C164304813 @default.
- W4383313391 hasConceptScore W4383313391C165205528 @default.
- W4383313391 hasConceptScore W4383313391C17409809 @default.
- W4383313391 hasConceptScore W4383313391C178790620 @default.
- W4383313391 hasConceptScore W4383313391C185592680 @default.
- W4383313391 hasConceptScore W4383313391C2776698055 @default.
- W4383313391 hasConceptScore W4383313391C2779227376 @default.
- W4383313391 hasConceptScore W4383313391C58097730 @default.
- W4383313391 hasConceptScore W4383313391C62520636 @default.
- W4383313391 hasConceptScore W4383313391C67236022 @default.
- W4383313391 hasConceptScore W4383313391C73462661 @default.
- W4383313391 hasConceptScore W4383313391C77928131 @default.
- W4383313391 hasConceptScore W4383313391C8058405 @default.
- W4383313391 hasConceptScore W4383313391C94436079 @default.
- W4383313391 hasIssue "9" @default.
- W4383313391 hasLocation W43833133911 @default.
- W4383313391 hasLocation W43833133912 @default.
- W4383313391 hasOpenAccess W4383313391 @default.
- W4383313391 hasPrimaryLocation W43833133911 @default.
- W4383313391 hasRelatedWork W2035325200 @default.