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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U-Pb thermochronology: creating a temporal record of lithosphere thermal evolution
TL;DR: In this paper, a new approach to U-Pb accessory mineral thermochronology was proposed to extract high-resolution time-temperature histories from lower crustal xenoliths.
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Rates and mechanisms of Mesoarchean magmatic arc construction, eastern Kaapvaal craton, Swaziland
TL;DR: A detailed study of a well-preserved Meso-archean crustal section from the oldest portion of the Kaapvaal craton, southern Africa, which records the complex interactions between deformation and magmatism during craton assembly ca. 3.3-3.2 Ga is presented in this paper.
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A stochastic sampling approach to zircon eruption age interpretation
TL;DR: In this article, a Bayesian approach was used to estimate the ages of magma eruption in the absence of independent confirmation that crystallization timescale is short relative to analytical uncertainties.
U-Pb geochronology of the Deccan Traps and relation to the end-Cretaceous mass extinction
Blair Schoene,Kyle M. Samperton,Michael P. Eddy,Gerta Keller,Thierry Adatte,Samuel A. Bowring,Syed F.R. Khadri,Brian Gertsch +7 more
TL;DR: U-Pb zircon geochronology is applied to Deccan rocks and it is shown that the main phase of eruptions initiated ~250,000 years before the Cretaceous-Paleogene boundary and that >1.1 million cubic kilometers of basalt erupted in ~750,000 Years.
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Disentangling the Hettangian carbon isotope record: Implications for the aftermath of the end-Triassic mass extinction
Annachiara Bartolini,Jean Guex,Jorge E. Spangenberg,Blair Schoene,D.G. Taylor,Urs Schaltegger,Viorel Atudorei +6 more
TL;DR: In this article, an organic carbon stable isotope (δ13Corg) record calibrated with detailed ammonite biostratigraphy, following the end-Triassic biological crisis is provided.