Petrology of arc volcanic rocks and their origin by mantle diapirs
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Light rare earth element depleted to enriched basaltic flows from 2.8 to 2.7 Ga greenstone belts of the Uchi Subprovince, Ontario, Canada
2006, Chemical GeologyCitation Excerpt :The two samples with Th/Ce close to or greater than 0.1 do not have lower Zr/Nb combined with greater La/Ybn compared to the remainder of the population, as would be expected for siliceous melts of sediments on a slab (Fig. 10; e.g., Elburg et al., 2002, and references therein). A decrease in the degree of partial melting is a consequence of a lower flux of water to the mantle wedge, longer fluid pathways to the zone of melting and greater depth of melting (Sakuyama, 1983; Tatsumi et al., 1991; Green, 1994; Barragan et al., 1998). There is a trend of increasing Nb content and La/Ybn, but decreasing Zr/Nb, from LKS through MKS to the alkaline lavas in this study (Tables 3 and 4).
Experimental constraints on differentiation and H<inf>2</inf>O abundance of calc-alkaline magmas
1996, Earth and Planetary Science LettersGeochemical characteristics of Sabalan volcanic rocks in Northwestern Iran
2019, Bulletin of the Mineral Research and Exploration
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