Item talk:Q269282
From geokb
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"name": "Tracing magmatic genesis and evolution through single zircon crystals from successive supereruptions from the Socorro Caldera Complex, USA",
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"abstract": "Large volume rhyolitic ignimbrite\u00a0volcanism\u00a0is a significant contributor to the evolving crust. The introduction of high-silica material into the\u00a0upper crust, differentiation within the middle crust, and partial melting in the\u00a0lower crust\u00a0contributes to geochemical and isotopic evolution of the crust. Developing accurate models for the genetic evolution of these events is dependent upon\u00a0geochronology\u00a0to determine rates of magmatic processes as model constraints. We present new\u00a0zircon\u00a0high-precision CA-ID-TIMS U-Pb geochronology and MC-ICPMS Hf\u00a0isotope geochemistry\u00a0for four ignimbrites from the nested caldera complex near Socorro, New Mexico (USA), within the Mogollon-Datil volcanic field. In agreement with past\u00a040Ar-39Ar data, interpretations of new U-Pb data indicate eruptions from the Socorro caldera cluster were pulsed. These pulses were intermittently spaced, and a volcanic hiatus following the Hells Mesa Tuff at 33.442 \u00b1 0.015 Ma was interrupted by four successive eruptions, beginning with the La Jencia Tuff at 29.158 \u00b1 0.025 Ma and finishing with the South Canyon Tuff at 28.066 \u00b1 0.021 Ma. Zircon age spectra became more protracted with each eruption, exhibiting age dispersions ranging from 0.347 Myr in the Hells Mesa Tuff to 4.502 Myr in the South Canyon Tuff. The increased dispersion is paralleled by an increase in the proportion of normally discordant grains, indicative of xenocryst incorporation. These protracted age spectra are not necessarily a function of thermal maturation in the middle to upper crust due to long-lived\u00a0magma\u00a0chambers. Rather, they are likely the result of increased melting of zircon-bearing lower crust due to deep thermal maturation from repeated juvenile magma injections based on the incorporation of zircon material at the melt source. In contrast, the Hf isotope record is volumetrically dominated by autocrystic zircon domains and becomes more radiogenic through time, recording juvenile\u00a0replenishment\u00a0of the lower crust during progressive melting. Together, these data record the protracted evolution of the lower crust sampled by ignimbrites, lend insight into that evolution, and emphasize the need for detailed interpretation of high-precision datasets to advance volcanic models.",
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