FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2337796562> ?p ?o ?g. }

• W2337796562 endingPage "1156" @default.
• W2337796562 startingPage "1153" @default.
• W2337796562 abstract "Despite the absence of ultrahigh-pressure (UHP) minerals such as coesite and microdiamond, Zhang et al. (2002a, 2002b) claimed to have found unambiguous evidence for UHP metamorphism in eclogites from the western Tianshan high-pressure (HP-LT) belt. UHP metamorphic rocks with an oceanic protolith provide evidence for the subduction of the oceanic lithosphere to mantle depths. If correct, these conclusions would demand a revision of previous tectonic models of northwestern China (e.g., Gao et al. 1995, 1998).However evidence for UHP eclogites is contradicted by the recent findings of Gao et al. (1999), Gao and Klemd (2000, 2001, 2003), and Klemd et al. (2002)—none of which was discussed by Zhang et al. (2002a, 2002b)—who estimated peak metamorphic conditions within the high-pressure eclogite-facies field. The equilibrium mineral assemblage of the eclogites and intimately interlayered garnet-omphacite blueschists from 25 different locations (Fig. 1⇓; including the three of Zhang et al. 2002a, 2002b) includes garnet-omphacite-rutile-quartz ± zoisite ± sodic-calcic to alkali amphiboles ± phengite ± paragonite. The eclogites only contain additional carbonates at two localities (Fig. 1⇓; also see Fig. 1⇓ in Zhang et al. 2002a). Using conventional exchange and net-transfer reactions (Gao et al. 1999; Gao and Klemd 2000, 2001, 2003; Klemd et al. 2002), as well as calculated PT-pseudosections for a specific bulk composition in the system NCFMASH (Klemd et al. 2002), peak conditions of 480 to 600 °C at 18–21 kbar were derived. Furthermore, Gao and Klemd (2001) suggested an isothermal decompression path as well as the presence of a low-salinity brine during HP-LT metamorphism.Although Zhang et al. (2002a, 2002b) only described three localities, they favored UHP conditions for all western Tianshan eclogites (see Abstract and Geological Implications in Zhang et …" @default.
• W2337796562 created "2016-06-24" @default.
• W2337796562 creator A5064629858 @default.
• W2337796562 date "2003-07-01" @default.
• W2337796562 modified "2023-10-03" @default.
• W2337796562 title "Ultrahigh-pressure metamorphism in eclogites from the western Tianshan high-pressure belt (Xinjiang, western China)-Comment" @default.
• W2337796562 cites W1500283396 @default.
• W2337796562 cites W1830358639 @default.
• W2337796562 cites W1856711543 @default.
• W2337796562 cites W1928320224 @default.
• W2337796562 cites W1982496504 @default.
• W2337796562 cites W1995549485 @default.
• W2337796562 cites W1997504854 @default.
• W2337796562 cites W2000649796 @default.
• W2337796562 cites W2006844676 @default.
• W2337796562 cites W2035542170 @default.
• W2337796562 cites W2042947244 @default.
• W2337796562 cites W2055208421 @default.
• W2337796562 cites W2060048441 @default.
• W2337796562 cites W2074514150 @default.
• W2337796562 cites W2096682995 @default.
• W2337796562 cites W2099670382 @default.
• W2337796562 cites W2116367855 @default.
• W2337796562 cites W2150773601 @default.
• W2337796562 cites W2157666617 @default.
• W2337796562 cites W2230819877 @default.
• W2337796562 cites W2244711968 @default.
• W2337796562 cites W2279147391 @default.
• W2337796562 cites W2340089515 @default.
• W2337796562 hasPublicationYear "2003" @default.
• W2337796562 type Work @default.
• W2337796562 sameAs 2337796562 @default.
• W2337796562 citedByCount "7" @default.
• W2337796562 countsByYear W23377965622012 @default.
• W2337796562 countsByYear W23377965622014 @default.
• W2337796562 countsByYear W23377965622019 @default.
• W2337796562 crossrefType "journal-article" @default.
• W2337796562 hasAuthorship W2337796562A5064629858 @default.
• W2337796562 hasConcept C109007969 @default.
• W2337796562 hasConcept C112764850 @default.
• W2337796562 hasConcept C114793014 @default.
• W2337796562 hasConcept C127313418 @default.
• W2337796562 hasConcept C140998209 @default.
• W2337796562 hasConcept C146588470 @default.
• W2337796562 hasConcept C151730666 @default.
• W2337796562 hasConcept C173347748 @default.
• W2337796562 hasConcept C17409809 @default.
• W2337796562 hasConcept C26687426 @default.
• W2337796562 hasConcept C2775974874 @default.
• W2337796562 hasConcept C2775988407 @default.
• W2337796562 hasConcept C2777054243 @default.
• W2337796562 hasConcept C2779508572 @default.
• W2337796562 hasConcept C2779870107 @default.
• W2337796562 hasConcept C4992710 @default.
• W2337796562 hasConcept C58097730 @default.
• W2337796562 hasConcept C5900021 @default.
• W2337796562 hasConcept C77928131 @default.
• W2337796562 hasConcept C79927612 @default.
• W2337796562 hasConcept C95628711 @default.
• W2337796562 hasConceptScore W2337796562C109007969 @default.
• W2337796562 hasConceptScore W2337796562C112764850 @default.
• W2337796562 hasConceptScore W2337796562C114793014 @default.
• W2337796562 hasConceptScore W2337796562C127313418 @default.
• W2337796562 hasConceptScore W2337796562C140998209 @default.
• W2337796562 hasConceptScore W2337796562C146588470 @default.
• W2337796562 hasConceptScore W2337796562C151730666 @default.
• W2337796562 hasConceptScore W2337796562C173347748 @default.
• W2337796562 hasConceptScore W2337796562C17409809 @default.
• W2337796562 hasConceptScore W2337796562C26687426 @default.
• W2337796562 hasConceptScore W2337796562C2775974874 @default.
• W2337796562 hasConceptScore W2337796562C2775988407 @default.
• W2337796562 hasConceptScore W2337796562C2777054243 @default.
• W2337796562 hasConceptScore W2337796562C2779508572 @default.
• W2337796562 hasConceptScore W2337796562C2779870107 @default.
• W2337796562 hasConceptScore W2337796562C4992710 @default.
• W2337796562 hasConceptScore W2337796562C58097730 @default.
• W2337796562 hasConceptScore W2337796562C5900021 @default.
• W2337796562 hasConceptScore W2337796562C77928131 @default.
• W2337796562 hasConceptScore W2337796562C79927612 @default.
• W2337796562 hasConceptScore W2337796562C95628711 @default.
• W2337796562 hasIssue "7" @default.
• W2337796562 hasLocation W23377965621 @default.
• W2337796562 hasOpenAccess W2337796562 @default.
• W2337796562 hasPrimaryLocation W23377965621 @default.
• W2337796562 hasRelatedWork W1579702023 @default.
• W2337796562 hasRelatedWork W1856711543 @default.
• W2337796562 hasRelatedWork W1984911596 @default.
• W2337796562 hasRelatedWork W1987046817 @default.
• W2337796562 hasRelatedWork W1989878389 @default.
• W2337796562 hasRelatedWork W1995549485 @default.
• W2337796562 hasRelatedWork W1997504854 @default.
• W2337796562 hasRelatedWork W2035542170 @default.
• W2337796562 hasRelatedWork W2041420592 @default.
• W2337796562 hasRelatedWork W2042947244 @default.
• W2337796562 hasRelatedWork W2046264604 @default.
• W2337796562 hasRelatedWork W2047550028 @default.
• W2337796562 hasRelatedWork W2060048441 @default.
• W2337796562 hasRelatedWork W2074514150 @default.

• next