B
Blair Schoene
Researcher at Princeton University
Publications - 118
Citations - 11770
Blair Schoene is an academic researcher from Princeton University. The author has contributed to research in topics: Zircon & Geochronology. The author has an hindex of 43, co-authored 101 publications receiving 9291 citations. Previous affiliations of Blair Schoene include Massachusetts Institute of Technology & University of Geneva.
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Ca and Mg isotope constraints on the origin of Earth's deepest δ13C excursion
TL;DR: In this paper, the authors present 257 δ 44 / 40 Ca and 131 δ 26 Mg measurements, along with [Mg], [Mn] and [Sr] data, from carbonates of the Ediacaran-aged Wonoka Formation (Fm.) of South Australia to bring new isotope systems to bear on understanding the Shuram excursion.
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Sm-Nd isotopic mapping of lithospheric growth and stabilization in the eastern Kaapvaal craton
TL;DR: This article used whole-rock Sm−Nd isotope systematics of 79 Archean granitoids from the eastern Kaapvaal craton, southern Africa, to delineate lithospheric boundaries and to constrain the timescale of crustal growth, assembly and geochemical differentiation.
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Zircon record of the plutonic-volcanic connection and protracted rhyolite melt evolution
Chad D. Deering,Brenhin Keller,Blair Schoene,Olivier Bachmann,Rachel J. Beane,Maria Ovtcharova +5 more
TL;DR: In this article, the potential petrogenetic link between a crystal-poor rhyolite (the Rhyolite Canyon Tuff) and its associated subvolcanic intrusion and crystal-rich post-caldera lavas from Turkey Creek, Arizona (USA), is examined using zircon chemical abrasion-thermal ionization mass spectrometry U-Pb geochronology and inductively coupled plasminetry trace element analyses.
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Evaluating the construction and evolution of upper crustal magma reservoirs with coupled U/Pb zircon geochronology and thermal modeling: A case study from the Mt. Capanne pluton (Elba, Italy)
TL;DR: In this article, high-precision ID-TIMS U-Pb zircon geochronology was combined with numerical thermal simulations to evaluate emplacement rates, test different emplacements models, inform zircoin age interpretations and evaluate the potential for melt storage during construction of the Mt. Capanne pluton.
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Short eruption window revealed by absolute crystal growth rates in a granitic magma
Mélanie Barboni,Blair Schoene +1 more
TL;DR: The authors showed that the magma solidified in the crust within just 10-40 thousand years of being injected into the crust, implying that the time window for an eruption was short.