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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Southern Africa
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Kaapvaal Craton (1)
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Europe
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Alps
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Piedmont Alps
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Dora Maira Massif (1)
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Western Alps
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Cottian Alps
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Dora Maira Massif (1)
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Mont Blanc (1)
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Southern Europe
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Italy
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Piemonte Italy
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Dora Maira Massif (1)
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Western Europe
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Cottian Alps
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Dora Maira Massif (1)
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elements, isotopes
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carbon
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C-13/C-12 (1)
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hydrogen (1)
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isotope ratios (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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metals
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alkaline earth metals
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calcium (1)
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oxygen (1)
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igneous rocks
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igneous rocks
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kimberlite (1)
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meteorites
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meteorites
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Acfer Meteorites (1)
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stony meteorites
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chondrites (1)
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minerals
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alloys (1)
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hydrates (2)
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minerals (2)
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native elements
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carbonado (1)
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diamond (1)
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oxides
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ilmenite (2)
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magnesium oxides (1)
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periclase (1)
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perovskite (3)
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silicates
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chain silicates
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pyroxene group
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clinopyroxene
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augite (1)
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diopside (1)
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framework silicates
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silica minerals
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coesite (3)
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quartz (5)
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stishovite (2)
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magnesian silicates (2)
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orthosilicates
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nesosilicates
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garnet group
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hydrogarnet (1)
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majorite (2)
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olivine group
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forsterite (7)
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olivine (5)
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ringwoodite (3)
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wadsleyite (2)
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sheet silicates
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mica group
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phlogopite (1)
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Primary terms
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Africa
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Southern Africa
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Kaapvaal Craton (1)
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carbon
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C-13/C-12 (1)
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crystal chemistry (1)
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crystal growth (4)
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crystal structure (13)
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data processing (2)
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deformation (17)
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Europe
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Alps
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Piedmont Alps
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Dora Maira Massif (1)
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Western Alps
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Cottian Alps
-
Dora Maira Massif (1)
-
-
Mont Blanc (1)
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-
-
Southern Europe
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Italy
-
Piemonte Italy
-
Dora Maira Massif (1)
-
-
-
-
Western Europe
-
Cottian Alps
-
Dora Maira Massif (1)
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-
-
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hydrogen (1)
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igneous rocks
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kimberlite (1)
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inclusions
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fluid inclusions (1)
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isotopes
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stable isotopes
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C-13/C-12 (1)
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magmas (1)
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mantle (12)
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metals
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alkaline earth metals
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calcium (1)
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metamorphism (2)
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meteorites
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Acfer Meteorites (1)
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stony meteorites
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chondrites (1)
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-
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minerals (2)
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oxygen (1)
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Complexions and stoichiometry of the 60.8°//[100](011) symmetrical tilt grain boundary in Mg 2 SiO 4 forsterite: A combined empirical potential and first-principles study
Application of scanning electron diffraction in the transmission electron microscope for the characterisation of dislocations in minerals
Continuous description of grain boundaries using crystal defect fields: the example of a {3 1 0}/[0 0 1] tilt boundary in MgO
Modeling dislocation glide and lattice friction in Mg 2 SiO 4 wadsleyite in conditions of the Earth’s transition zone
Acceptance of the Dana Medal of the Mineralogical Society of America for 2016
On the deformation mechanism of olivine single crystals at lithospheric temperatures: an electron tomography study
Decrease of hydrogen incorporation in forsterite from CO 2 -H 2 O-rich kimberlitic liquid
Transmission electron microscopy characterization of the dislocations and slip systems of the dense hydrous magnesium silicate superhydrous B
Origin of twist in ‘gwindel’ quartz crystals from the Alps: a transmission electron microscopy study
Characterization of dislocations and deformation processes by Transmission Electron Microscopy
Abstract Dislocations can be seen either as a linear domain of a crystal where atoms are misplaced, or through their long-range elastic strain fields. Transmission electron microscopy is sensitive to both aspects. Atomic-scale configurations within the dislocation cores can be imaged directly by high-resolution transmission electron microscopy and scanning transmission electron microscopy. On the other hand, the long-range lattice distortions induced in the crystal by dislocations give rise to a diffraction contrast in conventional transmission electron microscopy which can be used to image dislocation microstructures or to characterize their Burgers vectors. This chapter reviews the experimental techniques available in transmission electron microscopy to image and characterize dislocations.