HYDROLYTIC WEAKENING OF JADEITE IN UHP JADEITE-QUARTZITES FROM THE DABIE MOUNTAINS, EASTERN CHINA

dc.contributor.authorSu W.
dc.contributor.authorYe K.
dc.contributor.authorLiu J.
dc.date.accessioned2025-03-15T04:58:46Z
dc.date.available2025-03-15T04:58:46Z
dc.date.issued2006
dc.description.abstractDeformed jadeite grains in the UHP jadeite-quartzites from the Dabie Mountains, eastern China show evidence (by transmission electron microscopy, TEM) of plastic deformation: free dislocations, dislocation loops, dislocation networks, dislocation arrays and regularly spaced subgrain boundaries by dislocation walls. Electron energy-loss spectroscopy and TEM studies reveal the existence of water-rich bubbles within dislocations and imply a relationship with water-defect dislocation by water weakening in the jadeites. These observations suggest that the water-rich bubbles are a major weakening effect facilitating plastic deformation of jadeite by dislocation creep. © 2006 The Mineralogical Society.
dc.identifierhttps://elibrary.ru/item.asp?id=31411355
dc.identifier.citationMineralogical Magazine, 2006, 70, 5, 509-515
dc.identifier.doi10.1180/0026461067050354
dc.identifier.issn0026-461X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/48513
dc.subjectCHINA
dc.subjectDABIE MOUNTAINS
dc.subjectDEFORMATION MECHANISM
dc.subjectEELS
dc.subjectNATURAL JADEITE
dc.subjectTEM
dc.subjectWATER WEAKENING
dc.subjectWATER-RICH BUBBLES
dc.titleHYDROLYTIC WEAKENING OF JADEITE IN UHP JADEITE-QUARTZITES FROM THE DABIE MOUNTAINS, EASTERN CHINA
dc.typeСтатья

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