instrumental techniques applied to mineralogy and geochemistry

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16 Elisabetta Mariani et al FIGURE 3. Three feldspar patterns, a), b) and c) from a perthite grain indexed manually using Channel 5 Flamenco. Plagioclase 1 and K-Feldspar are the same orientation, plagioclase 2 exhibits an albite twin relationship with plagioclase 1 (180 around [201]). Also shown are the key differences from plagioclase 1 (on the right). Bands highlighted on plagioclase 1 are those that are not present in K-feldspar (green dashed) and plagioclase 2 (yellow dashed).
Electron backscatter diffraction (EBSD) in the SEM: applications to microstructures in minerals and rocks and recent technological advancements 17 FIGURE 4. a), b), c), d) and e) Omhpacite in Streaked Eclogite and f), g), h) and i) omphacite fan in undeformed eclogite, Colle della Barme d’Oropa, Sesia-Lanzo Zone, NW Italy. The Streaked Eclogite has a strong foliation defined by shape (omphacite and muscovite grains) and location (alternating bands of garnet and omphacite, plus quartz and muscovite) fabrics. Lineation is defined by quartz. Omphacite fans show large misorientations (up to 60°) across them (h). Pole figures show one single misorientation axes for the sub-grain boundaries (e and i). Only subtle chemical changes are observed (b and f).
Page 2 and 3: SEMINARIOS DE LA SOCIEDAD ESPAÑOLA
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