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Anorthosites mantle source

Seismic evidence for a mantle source for mid-Proterozoic anorthosites and implications for models of crustal growth... [Pg.125]

Whether derived from a mantle or crustal source, the origin of anorthosites must have left a distinct signature in the lower crust. The bulk composition of the lower crust is expected to be of gabbroic composition (metamorphosed in Grenville time) if the anorthosite magma was derived... [Pg.126]

The seismic properties of the Grenville lower crust are inconsistent with pyroxene-rich or high-grade metapelites (Fig. 2). This is crucial in determining which source, mantle or crust, is responsible for generating the mid-Proterozoic meta-anorthosites, as we will discuss below. [Pg.128]


See other pages where Anorthosites mantle source is mentioned: [Pg.125]    [Pg.125]    [Pg.127]    [Pg.128]    [Pg.130]    [Pg.132]    [Pg.132]    [Pg.132]    [Pg.133]    [Pg.585]    [Pg.586]    [Pg.126]   
See also in sourсe #XX -- [ Pg.125 , Pg.126 , Pg.127 , Pg.128 , Pg.129 , Pg.130 , Pg.131 , Pg.132 , Pg.133 ]




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