TRANSMISSION ELECTRON MICROSCOPY APPLIED TO FLUID INCLUSION INVESTIGATIONS

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dc.contributor.author Viti C.
dc.contributor.author Frezzotti M.L.
dc.date.accessioned 2021-02-09T05:17:58Z
dc.date.available 2021-02-09T05:17:58Z
dc.date.issued 2001
dc.identifier https://www.elibrary.ru/item.asp?id=516540
dc.identifier.citation Lithos, 2001, 55, 1-4, 125-138
dc.identifier.issn 0024-4937
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/24538
dc.description.abstract The transmission electron microscope (TEM) allows a detailed characterization of textural and chemical features of fluid inclusions (shape, inner compositions and inner textures), at a resolution higher than that attainable with an optical microscope (OM). TEM investigation indicates that most fluid inclusions appear as perfectly euhedral negative crystals, with variable shape (from prismatic to equant) and size (typically from <0.02 to 0.15 μm). Inner texture (fluid phase/melt distribution) and composition are variable as well. Different kinds of negative crystals may coexist in the same trail of inclusions, possibly indicating locally variable trapping conditions.A critical feature, revealed by TEM, is that inclusions are often connected to structural defects (in particular, to dislocation arrays), which are undetected by optical microscopy. The identification of these hidden nanostructures should be taken into account for the correct petrological interpretation of microthermometric results, particularly when controversial data have been obtained. In fact, these nanostructures may represent a possible path for fluid phase leakage, thus modifying the original composition and/or density of the inclusions.
dc.subject TEM
dc.subject FLUID INCLUSIONS
dc.subject NEGATIVE CRYSTALS
dc.subject DISLOCATIONS
dc.subject LEAKAGE
dc.subject RE-EQUILIBRATION
dc.title TRANSMISSION ELECTRON MICROSCOPY APPLIED TO FLUID INCLUSION INVESTIGATIONS
dc.type Статья


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