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Orogenic peridotite massifs trace elements

The distribution of lithophile trace elements (REE + mbidium, caesium, strontium, barium, yttrium, zirconium, hafnium, niobium, tantalum, thorium, and uranium) normalized to primitive mantle (PM) values are illustrated in Figure 16 for a range of peridotite lithologies from the Ronda orogenic Iherzolite massif, and in Figure 17 for ophiolitic and abyssal refractory peridotites. [Pg.834]

Figure 16 Abundances of lithophile trace elements normalized to PM values in orogenic peridotites from the Ronda massif (whole-rock analyses). Data from Remaidi (1993). Normalizing values after Sun and McDonough (1989). Figure 16 Abundances of lithophile trace elements normalized to PM values in orogenic peridotites from the Ronda massif (whole-rock analyses). Data from Remaidi (1993). Normalizing values after Sun and McDonough (1989).
See other pages where Orogenic peridotite massifs trace elements is mentioned: [Pg.814]    [Pg.838]    [Pg.849]    [Pg.112]    [Pg.136]    [Pg.147]   
See also in sourсe #XX -- [ Pg.200 , Pg.201 , Pg.205 ]



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