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bytownite, once a valid species name, is now an informal term used for plagioclase feldspar with anorthite/albite ratios in the range 70:30 to 90:10. It is an important rock-forming mineral in basic composition igneous rocks such as gabbros and basalts.
the effects of low-temperature alteration have resulted in much bytownite being replaced by more sodic plagioclase, most notably albite. Greenly (1919) reported the mineral from the ‘post-Carboniferous’ (Palaeogene) dykes from Anglesey, although no specific localities are referred to. Hawkins (1970) & Cattermole (1976) both describe bytownite in the Rhiw Intrusion, Llŷn, although identifications were made on the basis of optical properties of the mineral. Similar optical determination of bytownite has been made by Archer & Elliott (1965) from olivine dolerite dykes from Parc Mine, near Llanrwst and by Roach (1969) in some gabbros of the St. David’s Head Intrusion. The latter occurrence has been confirmed by microprobe analyses.