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Uploaded on:
2009-03-12 10:00:00.0
Type:
Digital Asset
File Size:
217.48 KB
Dimensions:
1000 x 667 pixels
145 views 4 downloads
P number: P524229
Caption: Photomicrograph of felsic porphyrite. Light: PPL, Magnification x 2. 850 feet at 126 degrees from Cougie, Glen Affric, Invernessshire.
Description: The image is a photomicrograph of a thin section of a felsic porphyrite, containing large phenocrysts of clear feldspar within a fine-grained granular matrix of quartz and feldspar with abundant small flakes of dark-coloured biotite mica. British Geological Survey Petrology Collection sample number S 56759. Light: PPL, Magnification x 2. Light: PPL, Magnification x 2. The term porphyrite has long been used by petrologists for a rock which is more correctly called a porphyritic microdiorite. Some of the porphyrites surrounding the Criffel-Dalbeattie granite in south-west Scotland consist of a devitrified glassy matrix in which the abundant and relatively large phenocrysts are embedded. Most of these rocks are intrusive in origin. The felsic porphyrites are a set of minor intrusions associated with the Caledonian Orogeny, they are late- to post-tectonic. They are mostly porphyritic microgranites with phenocrysts of oscillatory-zoned albite-oligoclase, biotite and in places hornblende set in a granoblastic fine-grained groundmass of quartz, potash feldspar and acid plagioclase in equal proportions. They are commonly schistose having been deformed and recrystallized to produce amphibolite or greenschist-facies mineral assemblages.
Date taken: Wed Jan 01 00:00:00 GMT 2003
Photographer: Hyslop, E.K.
Copyright statement: NERC
X longitude/easting: 224400
Y latitude/northing: 821000
Coordinate reference system, ESPG code: 27700 (OSGB 1936 / British National Grid)
Orientation: Landscape
Size: 217.48 KB; 1000 x 667 pixels; 85 x 56 mm (print at 300 DPI); 265 x 176 mm (screen at 96 DPI);
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