Trace elements in minerals from mafic and ultramafic cumulates of the central Sierra de Valle Fértil, Famatinian arc, Argentina

• Published in: Lithos Vol. 240-243; pp. 355 - 370
• Main Authors: Otamendi, Juan E., Tiepolo, Massimo, Walker, Barry A., Cristofolini, Eber A., Tibaldi, Alina M.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.01.2016
• Subjects: Arc; Cumulate; Famatinian arc; Magmatism; Trace element; Argentina; Magmatism; Trace element; Arc; Cumulate; Famatinian arc
• ISSN: 0024-4937; 1872-6143
• DOI: 10.1016/j.lithos.2015.11.009

Trace element abundances in constituent minerals from mafic and ultramafic rocks of a deep arc crustal section are studied to observe their abundance and distribution. Five cumulate rocks were selected from a sequence that consists of pyroxene hornblende peridotite, olivine hornblende gabbronorite, pyroxene hornblende gabbronorite, hornblende gabbronorite, gabbro and anorthosite. Solid/liquid partition coefficients calculated with the equilibrium distribution model indicate that Cr, Ni, Co, Zn and V are highly compatible with an olivine-dominated mineral assemblage from the mafic and ultramafic cumulates. The compatibility of Ti and Sc would be dependent on the stability of clinopyroxene, amphibole and oxides in the magmatic system. With few exceptions, the other trace elements are incompatible with the minerals that form the cumulate. At most half the mass of Sr carried by a primitive arc magma could be stored in anorthite-rich plagioclase from the mafic cumulates. Magmatic amphibole fractionates Y, middle and heavy REE from other incompatible elements during crystal accumulation of mafic cumulates. In contrast, late magmatic to subsolidus amphibole has no effect on the differentiation of a primitive arc magma. In fact, the trace element variability of amphibole and clinopyroxene is easily related to different stages of magmatic evolution within the cumulate pile. The results presented here are helpful for modelling other cases of arc magma petrogenesis where the cumulate rocks with dominant mafic assemblages are not exposed. •Trace element abundances in minerals from arc cumulate rocks•Trace elemental variation in minerals reveals different degrees of compatibility.•Calculation of partition coefficients using concentration in minerals•Amphibole and clinopyroxene are the predominant repositories of trace elements.