Matches in SemOpenAlex for { <https://semopenalex.org/work/W2159142807> ?p ?o ?g. }
- W2159142807 endingPage "1015" @default.
- W2159142807 startingPage "991" @default.
- W2159142807 abstract "The P–T gradient in a Late Eocene low-T high-P metamorphic belt in northern New Caledonia increases from SW to NE. Metapelites in the pumpellyite–prehnite and blueschist zones contain lawsonite, Mg-carpholite, Fe-stilpnomelane and Fe-glaucophane. Thermodynamic calculations indicate a progression of metamorphic conditions from less than 0·3 GPa and 250°C in a kaolinite-bearing rock in the SW, up to 1·5 GPa and 410°C in a lawsonite–glaucophane-bearing sample in the NE of the Diahot terrane. Through a multi-method investigation of phyllosilicates, organic matter and fluid inclusions, we demonstrate that the evolution of organic matter and illite crystallinity depends strongly on the evolution of the P–T path with time. In addition, we show that the illite–muscovite b cell dimension provides a robust estimate of maximum pressure reached in low-temperature domains with polyphase metamorphic histories, despite subsequent high-temperature–low-pressure events. Fluid inclusion study reveals an isothermal decompression in the Diahot terrane." @default.
- W2159142807 created "2016-06-24" @default.
- W2159142807 creator A5007404892 @default.
- W2159142807 creator A5036362259 @default.
- W2159142807 creator A5067573831 @default.
- W2159142807 creator A5074746034 @default.
- W2159142807 creator A5086541232 @default.
- W2159142807 date "2006-02-21" @default.
- W2159142807 modified "2023-09-27" @default.
- W2159142807 title "Very Low-grade Metamorphic Evolution of Pelitic Rocks under High-pressure/Low-temperature Conditions, NW New Caledonia (SW Pacific)" @default.
- W2159142807 cites W1219489599 @default.
- W2159142807 cites W1535489635 @default.
- W2159142807 cites W1574610338 @default.
- W2159142807 cites W1595216972 @default.
- W2159142807 cites W1972423246 @default.
- W2159142807 cites W1973395603 @default.
- W2159142807 cites W1979148496 @default.
- W2159142807 cites W1979863231 @default.
- W2159142807 cites W1983554365 @default.
- W2159142807 cites W1988738923 @default.
- W2159142807 cites W1990294778 @default.
- W2159142807 cites W1992524555 @default.
- W2159142807 cites W2004903824 @default.
- W2159142807 cites W2012512655 @default.
- W2159142807 cites W2016456230 @default.
- W2159142807 cites W2020587493 @default.
- W2159142807 cites W2020639025 @default.
- W2159142807 cites W2027171096 @default.
- W2159142807 cites W2032544550 @default.
- W2159142807 cites W2032908701 @default.
- W2159142807 cites W2039817695 @default.
- W2159142807 cites W2054643770 @default.
- W2159142807 cites W2055071952 @default.
- W2159142807 cites W2060847682 @default.
- W2159142807 cites W2065255360 @default.
- W2159142807 cites W2067265405 @default.
- W2159142807 cites W2067685831 @default.
- W2159142807 cites W2073250859 @default.
- W2159142807 cites W2079942975 @default.
- W2159142807 cites W2081149290 @default.
- W2159142807 cites W2082266522 @default.
- W2159142807 cites W2082645751 @default.
- W2159142807 cites W2082767849 @default.
- W2159142807 cites W2087261379 @default.
- W2159142807 cites W2088779208 @default.
- W2159142807 cites W2091143840 @default.
- W2159142807 cites W2094917496 @default.
- W2159142807 cites W2104139642 @default.
- W2159142807 cites W2106076755 @default.
- W2159142807 cites W2113578304 @default.
- W2159142807 cites W2129143054 @default.
- W2159142807 cites W2135124879 @default.
- W2159142807 cites W2136501354 @default.
- W2159142807 cites W2153647299 @default.
- W2159142807 cites W2159913816 @default.
- W2159142807 cites W2326306154 @default.
- W2159142807 cites W2330756480 @default.
- W2159142807 cites W2340022951 @default.
- W2159142807 cites W2406687541 @default.
- W2159142807 cites W2601144783 @default.
- W2159142807 cites W2975652074 @default.
- W2159142807 cites W3081662087 @default.
- W2159142807 cites W4235578445 @default.
- W2159142807 cites W4240062274 @default.
- W2159142807 cites W4248940735 @default.
- W2159142807 doi "https://doi.org/10.1093/petrology/egl001" @default.
- W2159142807 hasPublicationYear "2006" @default.
- W2159142807 type Work @default.
- W2159142807 sameAs 2159142807 @default.
- W2159142807 citedByCount "56" @default.
- W2159142807 countsByYear W21591428072012 @default.
- W2159142807 countsByYear W21591428072013 @default.
- W2159142807 countsByYear W21591428072015 @default.
- W2159142807 countsByYear W21591428072016 @default.
- W2159142807 countsByYear W21591428072017 @default.
- W2159142807 countsByYear W21591428072018 @default.
- W2159142807 countsByYear W21591428072020 @default.
- W2159142807 countsByYear W21591428072021 @default.
- W2159142807 countsByYear W21591428072022 @default.
- W2159142807 countsByYear W21591428072023 @default.
- W2159142807 crossrefType "journal-article" @default.
- W2159142807 hasAuthorship W2159142807A5007404892 @default.
- W2159142807 hasAuthorship W2159142807A5036362259 @default.
- W2159142807 hasAuthorship W2159142807A5067573831 @default.
- W2159142807 hasAuthorship W2159142807A5074746034 @default.
- W2159142807 hasAuthorship W2159142807A5086541232 @default.
- W2159142807 hasBestOaLocation W21591428071 @default.
- W2159142807 hasConcept C127313418 @default.
- W2159142807 hasConcept C150999391 @default.
- W2159142807 hasConcept C151730666 @default.
- W2159142807 hasConcept C171710264 @default.
- W2159142807 hasConcept C173347748 @default.
- W2159142807 hasConcept C17409809 @default.
- W2159142807 hasConcept C26687426 @default.
- W2159142807 hasConcept C2776581184 @default.
- W2159142807 hasConcept C2777054243 @default.
- W2159142807 hasConcept C2779429093 @default.
- W2159142807 hasConcept C2779508572 @default.