Abstract
During solidification of magma chambers as systems closed to chemical exchange with environs, the residual siliceous melt may follow a trend of rising, constant, or decreasing oxidation state, relative to reference buffers such as nickel + nickel oxide (NNO) or fayalite + magnetite + quartz. Titanomagnetite–hemoilmenite thermometry and oxybarometry on quenched volcanic suites yield temperature versus oxygen fugacity arrays of varied positive and negative slopes, the validity of which has been disputed for several years. We resolve the controversy by introducing a new recorder of magmatic redox evolution employing temperature- and redox-sensitive trace-element abundances in zircon. The zircon/melt partition coefficients of cerium and uranium vary oppositely in response to variation of magma redox state, but vary in tandem as temperature varies. Plots of U/Pr versus Ce4+/Ce3+ in zircon provide a robust test for change in oxidation state of the melt during zircon crystallisation from cooling magma, and the plots discriminate thermally induced from redox-induced variation of Ce4+/Ce3+ in zircon. Temperature-dependent lattice strain causes Ce4+/Ce3+ in zircon to increase strongly as zircon crystallises from cooling magma at constant Ce4+/Ce3+ ratio in the melt. We examine 19 zircon populations from igneous complexes in varied tectonic settings. Variation of zircon Ce4+/Ce3+ due to minor variation in melt oxidation state during crystallisation is resolvable in 11 cases but very subordinate to temperature dependence. In many zircon populations described in published literature, there is no resolvable change in redox state of the melt during tenfold variation of Ce4+/Ce3+ in zircons. Varied magmatic redox trends indicated by different slopes on plots of zircon U/Pr versus Ce4+/Ce3+ are corroborated by Fe–Ti-oxide-based T–ƒO2 trends of correspondingly varied slopes. Zircon and Fe–Ti-oxide compositions agree that exceptionally, H2O-rich arc magmas tend to follow a trend of rising oxidation state of the melt during late stages of fluid-saturated magmatic differentiation at upper-crustal pressures. We suggest that H2 and/or SO3 and/or Fe2+ loss from the melt to segregating fluid is largely responsible. Conversely, zircon and Fe–Ti-oxide compositions agree in indicating that H2O-poor magmas tend to follow a T–ƒO2 trend of decreasing oxidation state of the melt during late stages of magmatic differentiation at upper-crustal pressures, because the precipitating mineral assemblage has higher Fe3+/Fe2+ than coexisting rhyolitic melt. We present new evidence showing that the Fe–Ti-oxide oxybarometer calibration by Ghiorso and Evans (Am J Sci 308(9):957–1039, 2008) retrieves experimentally imposed values of ƒO2 in laboratory syntheses of Fe–Ti-oxide pairs to a precision of ± 0.2 log unit, over a large experimental temperature range, without systematic bias up to at least log ƒO2 ≈ NNO + 4.4. Their titanomagnetite–hemoilmenite geothermometer calibration has large systematic errors in application to Ti-poor oxides that precipitate from very oxidised magmas. A key outcome is validation of Fe–Ti-oxide-based values of melt TiO2 activity for use in Ti-in-zircon thermometry and Ti-in-quartz thermobarometry.
Highlights
Accurate geothermometry is a key that often unlocks access to other geologically useful information from chemically analysed glass and/or mineral assemblages—e.g., rock or magma viscosity, pressure of crystallisation and depth of1 3 Vol.:(0123456789) 104 Page 2 of 21Contributions to Mineralogy and Petrology (2018) 173:104 subsequent erosional exhumation, oxygen or sulphur fugacity, or the dissolved H 2O content in a magma
This work presents new evidence that shows that the Fe–Ti-oxide oxybarometer calibration by Ghiorso and Evans (2008) retrieves experimentally imposed values of ƒO2 in laboratory syntheses of Fe–Ti-oxide pairs to a precision of ± 0.2 log unit, over a large experimental temperature range, without systematic bias up to at least log ƒO2 ≈ nickel + nickel oxide (NNO) + 4.4
In many natural assemblages described in published literature and interpreted as redox indicators, there is no resolvable change in redox state of the melt over a large range of Ce4+/Ce3+ variation in zircons
Summary
Accurate geothermometry is a key that often unlocks access to other geologically useful information from chemically analysed glass and/or mineral assemblages—e.g., rock or magma viscosity, pressure of crystallisation and depth of1 3 Vol.:(0123456789) 104 Page 2 of 21Contributions to Mineralogy and Petrology (2018) 173:104 subsequent erosional exhumation, oxygen or sulphur fugacity, or the dissolved H 2O content in a magma. Dispersion of zircon and Fe–Ti-oxide compositions within volcanic suites is in many cases due in part to chamber replenishments and magma mixing immediately preceding the eruptions, as documented for the Bishop Tuff, Younger Toba Tuff, and Yellowstone supereruptions, among others (Evans and Bachmann 2013; Chesner and Luhr 2010; Wotzlaw et al 2015).
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