Redox and structural controls on tin isotopic fractionations among magmas

Journal Article · Tue Oct 01 00:00:00 EDT 2019 · Geochimica et Cosmochimica Acta

DOI:https://doi.org/10.1016/j.gca.2019.09.036· OSTI ID:1577104

Roskosz, M. ^[1]; Amet, Q. ^[2]; Fitoussi, C. ^[2]; Dauphas, N.  ^[3]; Bourdon, B.  ^[2]; Tissandier, L. ^[4]; Hu, M. Y. ^[5]; Said, A. ^[5]; Alatas, A. ^[5]; Alp, E. E. ^[5]

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1. Sorbonne Univ., Paris (France); Universite Pierre et Marie Curie, Paris (France)
2. Claude Bernard Univ. Lyon (UCBL) (France); Centre National de la Recherche Scientifique (CNRS), Lyon (France)
3. Univ. of Chicago, IL (United States)
4. Universite de Lorraine, Vandoeuvre-les-Nancy (France); Centre National de la Recherche Scientifique (CNRS), Vandoeuvre-les-Nancy (France)
5. Argonne National Lab. (ANL), Argonne, IL (United States). Advanced Photon Source (APS)

Recent analytical developments have made possible the determination of the isotopic composition of tin in igneous rocks. In order to establish a framework to interpret the mass-dependent tin isotopic signatures of planetary materials, in this work, seven geologically-relevant silicate glasses (basalt, rhyolite, enstatite and anorthite glasses) were synthesized with moderate amounts of ¹¹⁹Sn (on the order of a weight percent). Redox conditions were controlled during sample synthesis to set the redox ratio (Sn²⁺/Sn_tot) from stannous (Sn²⁺) to stannic (Sn⁴⁺) glasses. The mean force constants of tin bonds in these glasses were determined by synchrotron nuclear resonant inelastic X-ray scattering (NRIXS) in order to determine the reduced isotopic partition function ratios (β-factors) of these glasses. Clues on the coordination chemistry and the valence state of tin in these glasses were also derived from synchrotron Mossbauer spectroscopy (SMS). The force constants of tin drastically increases from Sn²⁺-bearing to Sn⁴⁺-bearing glasses and varies significantly with the glass composition at a given redox state. The average coordination number of tin likely controls these variations with glass composition as suggested by SMS results. It is concluded that large isotope fractionation is expected between materials containing Sn²⁺ and Sn⁴⁺ respectively even at magmatic temperatures and that the coordination chemistry of tin in silicates strongly affect its isotope partitioning behavior. Our experimental data are finally used to interpret available Sn isotope data collected in terrestrial rocks. The incompatible behavior of Sn⁴⁺ in mantle minerals leads to a enrichment in heavy isotopes in mantle melts and to the depletion in heavy isotopes in solid residues of melting with a magnitude consistent with the isotope fractionation between Sn²⁺ and Sn⁴⁺ predicted by NRIXS data. Finally, we show that during fractional crystallization of basalt and considering the effect of tin coordination number in minerals and melts, the partitioning of Sn⁴⁺ into ilmenite leads to an enrichment in light isotopes in the residual melt.

• Research Organization: Argonne National Lab. (ANL), Argonne, IL (United States). Advanced Photon Source (APS)
• Sponsoring Organization: USDOE Office of Science (SC), Basic Energy Sciences (BES); France And Chicago Collaborating in The Sciences (FACCTS); National Aeronautics and Space Administration (NASA)
• Grant/Contract Number: AC02-06CH11357; FACCTS 2015-173-N0; NNX17AE86G; NNX17AE87G; NSSC17K0744
• OSTI ID: 1577104
• Journal Information: Geochimica et Cosmochimica Acta, Vol. 268; ISSN 0016-7037
• Publisher: Elsevier; The Geochemical Society; The Meteoritical Society
• Country of Publication: United States
• Language: English

Related Subjects

58 GEOSCIENCES
Magma differentiation
Mantle melting
Silicate melts
Tin isotopes