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Subduction zones basalt compositions

Ono S. (1998) Stability limits of hydrous minerals in sediment and mid-ocean ridge basalt compositions implications for water transport in subduction zones. J. Geophys. Res. 103, 18253-18267. [Pg.1168]

Using average MORE or the range of compositions of oceanic basalts (e.g., Hofmann, 1988 Chapter 3.13 and http //petdb.ldeo.columbia.edu Lehnert et al., 2000), the fluxes derived here can be applied to determine the average compositions of oceanic crust that is subducted and recycled into the mantle. These compositions thus influence the composition of subduction zone magmas (see Chapter 3.18) and bear on the chemical mass balance of the mantle. [Pg.1790]

See other pages where Subduction zones basalt compositions is mentioned: [Pg.506]    [Pg.750]    [Pg.1007]    [Pg.1151]    [Pg.1161]    [Pg.1192]    [Pg.1352]    [Pg.1773]    [Pg.1790]    [Pg.1843]    [Pg.1903]    [Pg.22]    [Pg.46]    [Pg.306]    [Pg.452]    [Pg.462]    [Pg.494]    [Pg.605]    [Pg.264]    [Pg.334]    [Pg.345]    [Pg.532]    [Pg.11]    [Pg.175]    [Pg.123]    [Pg.363]    [Pg.8]    [Pg.269]   
See also in sourсe #XX -- [ Pg.45 ]



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