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Mafic enclaves

Fig. 2.7. Mantle normalised incompatible element patterns of representative Tuscany mafic rocks (A, B) and for mafic enclaves hosted by silicic rocks (C). The field of Aeolian arc calc-alkaline and shoshonitic mafic rocks is shown for comparison. Fig. 2.7. Mantle normalised incompatible element patterns of representative Tuscany mafic rocks (A, B) and for mafic enclaves hosted by silicic rocks (C). The field of Aeolian arc calc-alkaline and shoshonitic mafic rocks is shown for comparison.
Petrological and geochemical signatures of mafic enclaves match quite closely those of the Tuscany mafic rocks. However, some of the observed geochemical characteristics may have been modified by interaction with host silicic magmas and could not represent pristine compositions of mafic melts. [Pg.38]

Brigatti MF, Lugli C, Poppi L, Elburg M (1998b) Crystal chemistry of biotites from mafic enclaves in the Warburton granodiorite, Lachlan Fold Belt (Australia). Eur J Mineral 10 855-864... [Pg.91]

See other pages where Mafic enclaves is mentioned: [Pg.26]    [Pg.26]    [Pg.28]    [Pg.29]    [Pg.29]    [Pg.30]    [Pg.30]    [Pg.33]    [Pg.37]    [Pg.37]    [Pg.38]    [Pg.39]    [Pg.39]    [Pg.193]    [Pg.197]    [Pg.1632]    [Pg.1657]    [Pg.256]    [Pg.287]    [Pg.26]    [Pg.26]    [Pg.28]    [Pg.29]    [Pg.29]    [Pg.30]    [Pg.30]    [Pg.33]    [Pg.37]    [Pg.37]    [Pg.38]    [Pg.39]    [Pg.39]    [Pg.193]    [Pg.197]    [Pg.1632]    [Pg.1657]    [Pg.256]    [Pg.287]    [Pg.182]    [Pg.24]    [Pg.29]    [Pg.31]    [Pg.194]    [Pg.195]    [Pg.1564]    [Pg.1564]    [Pg.1634]    [Pg.1649]    [Pg.1649]    [Pg.1656]    [Pg.1657]    [Pg.1657]    [Pg.255]   
See also in sourсe #XX -- [ Pg.37 , Pg.39 ]



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