Grain size of plagioclase of the basaltic andesite dikes, Iritono, central Abukuma plateau
1977 ◽
Vol 14
(8)
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pp. 1860-1866
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The width (W) of plagioclase crystallizing from magmas is given by the equation log [Formula: see text] where t is the crystallization time calculated from Jaeger's model and η is the viscosity of a magma. The values log 2η−1/3 for basaltic and granitic magmas under hydrous and anhydrous conditions are −0.1 and −1.0 for basaltic magmas, and −1.5 and −3.5 for granitic magmas, respectively. The equation can be explained by coarsening, thermal diffusion, and (or) material diffusion processes.
2014 ◽
Vol 0
(s5)
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pp. 45-55
Keyword(s):
1977 ◽
Keyword(s):
2007 ◽
Vol 43
(5)
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pp. 590-594
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