FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2015193526> ?p ?o ?g. }

• W2015193526 endingPage "732" @default.
• W2015193526 startingPage "719" @default.
• W2015193526 abstract "It has been often debated whether all granitic gneisses associated with coesite‐bearing eclogites in southern Dabieshan, China, have also been subjected to ultrahigh‐pressure (UHP) metamorphism. We show here that a metagranitoid adjacent to the Bixiling eclogite‐ultramafic complex has preserved primary granitic textures and an igneous mineral assemblage of $$mathrm{biotite},+mathrm{plagioclase},+mathrm{microcline},+mathrm{quartz},+mathrm{allanite},pm mathrm{amphibole},$$. The absence of UHP recrystallization for the metagranitoid is particularly manifested by the conservation of euhedral‐zoned plagioclase phenocrysts, the lack of corona garnets around igneous biotite, and the presence of an igneous mineral assemblage in zircons. The only metamorphic overprint was the epidote‐amphibolite facies metamorphism characterized by the assemblage of $$mathrm{biotite},+mathrm{phengiticmica},+mathrm{epidote},+mathrm{albite},+mathrm{K},- mathrm{feldspar},+mathrm{quartz},pm mathrm{amphibole},$$. Metamorphic conditions are estimated at ca. 550°–680°C and 6–13 kbar for the metagranitoid and its amphibolitic enclave. Geochemically, the metagranitoid is similar to its country gneiss and shows an affinity to volcanic arc granitoid. Zircon U‐Pb dating suggests that the Bixiling metagranitoid was emplaced during the Neoproterozoic ($$729pm 4$$ Ma), when most other granitic rocks and the protoliths of eclogite were also formed in Dabieshan. Taking into account the discovery of non‐UHP granitic gneisses in other places, we argue that part of Neoproterozoic granitic rocks in the Dabieshan and Sulu terranes have escaped UHP metamorphism during the Triassic deep subduction of the continental crust as a consequence of a lack of penetrative deformation and fluid‐rock interaction." @default.
• W2015193526 created "2016-06-24" @default.
• W2015193526 creator A5031219380 @default.
• W2015193526 creator A5046706991 @default.
• W2015193526 creator A5047575196 @default.
• W2015193526 creator A5060414536 @default.
• W2015193526 creator A5082519097 @default.
• W2015193526 date "2003-11-01" @default.
• W2015193526 modified "2023-10-18" @default.
• W2015193526 title "Neoproterozoic Granitoid Did Not Record Ultrahigh‐Pressure Metamorphism from the Southern Dabieshan of China" @default.
• W2015193526 cites W1512836224 @default.
• W2015193526 cites W1972673996 @default.
• W2015193526 cites W1972715171 @default.
• W2015193526 cites W1973395603 @default.
• W2015193526 cites W1974258910 @default.
• W2015193526 cites W1977457396 @default.
• W2015193526 cites W1985297387 @default.
• W2015193526 cites W1990832196 @default.
• W2015193526 cites W1994209198 @default.
• W2015193526 cites W2005168810 @default.
• W2015193526 cites W2005434102 @default.
• W2015193526 cites W2015061860 @default.
• W2015193526 cites W2019877001 @default.
• W2015193526 cites W2021345743 @default.
• W2015193526 cites W2028642961 @default.
• W2015193526 cites W2029286864 @default.
• W2015193526 cites W2031317963 @default.
• W2015193526 cites W2040549377 @default.
• W2015193526 cites W2040903195 @default.
• W2015193526 cites W2048505147 @default.
• W2015193526 cites W2049191257 @default.
• W2015193526 cites W2052973516 @default.
• W2015193526 cites W2053422899 @default.
• W2015193526 cites W2054066569 @default.
• W2015193526 cites W2062578168 @default.
• W2015193526 cites W2071369893 @default.
• W2015193526 cites W2073326270 @default.
• W2015193526 cites W2075170239 @default.
• W2015193526 cites W2102351976 @default.
• W2015193526 cites W2106146079 @default.
• W2015193526 cites W2107300066 @default.
• W2015193526 cites W2108971421 @default.
• W2015193526 cites W2141890535 @default.
• W2015193526 cites W2162860634 @default.
• W2015193526 cites W2338345412 @default.
• W2015193526 cites W2598678755 @default.
• W2015193526 cites W2922460553 @default.
• W2015193526 doi "https://doi.org/10.1086/378336" @default.
• W2015193526 hasPublicationYear "2003" @default.
• W2015193526 type Work @default.
• W2015193526 sameAs 2015193526 @default.
• W2015193526 citedByCount "16" @default.
• W2015193526 countsByYear W20151935262012 @default.
• W2015193526 countsByYear W20151935262015 @default.
• W2015193526 countsByYear W20151935262016 @default.
• W2015193526 countsByYear W20151935262019 @default.
• W2015193526 countsByYear W20151935262020 @default.
• W2015193526 countsByYear W20151935262021 @default.
• W2015193526 countsByYear W20151935262022 @default.
• W2015193526 countsByYear W20151935262023 @default.
• W2015193526 crossrefType "journal-article" @default.
• W2015193526 hasAuthorship W2015193526A5031219380 @default.
• W2015193526 hasAuthorship W2015193526A5046706991 @default.
• W2015193526 hasAuthorship W2015193526A5047575196 @default.
• W2015193526 hasAuthorship W2015193526A5060414536 @default.
• W2015193526 hasAuthorship W2015193526A5082519097 @default.
• W2015193526 hasConcept C109007969 @default.
• W2015193526 hasConcept C112764850 @default.
• W2015193526 hasConcept C127313418 @default.
• W2015193526 hasConcept C141646446 @default.
• W2015193526 hasConcept C146588470 @default.
• W2015193526 hasConcept C151730666 @default.
• W2015193526 hasConcept C171701179 @default.
• W2015193526 hasConcept C173347748 @default.
• W2015193526 hasConcept C17409809 @default.
• W2015193526 hasConcept C26687426 @default.
• W2015193526 hasConcept C2775974874 @default.
• W2015193526 hasConcept C2776698055 @default.
• W2015193526 hasConcept C2778849375 @default.
• W2015193526 hasConcept C42787717 @default.
• W2015193526 hasConcept C58097730 @default.
• W2015193526 hasConcept C5900021 @default.
• W2015193526 hasConcept C77928131 @default.
• W2015193526 hasConcept C79927612 @default.
• W2015193526 hasConcept C95628711 @default.
• W2015193526 hasConceptScore W2015193526C109007969 @default.
• W2015193526 hasConceptScore W2015193526C112764850 @default.
• W2015193526 hasConceptScore W2015193526C127313418 @default.
• W2015193526 hasConceptScore W2015193526C141646446 @default.
• W2015193526 hasConceptScore W2015193526C146588470 @default.
• W2015193526 hasConceptScore W2015193526C151730666 @default.
• W2015193526 hasConceptScore W2015193526C171701179 @default.
• W2015193526 hasConceptScore W2015193526C173347748 @default.
• W2015193526 hasConceptScore W2015193526C17409809 @default.
• W2015193526 hasConceptScore W2015193526C26687426 @default.
• W2015193526 hasConceptScore W2015193526C2775974874 @default.
• W2015193526 hasConceptScore W2015193526C2776698055 @default.
• W2015193526 hasConceptScore W2015193526C2778849375 @default.

• next