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John O. Stone

Researcher at University of Washington

Publications -  101
Citations -  10453

John O. Stone is an academic researcher from University of Washington. The author has contributed to research in topics: Ice sheet & Glacial period. The author has an hindex of 46, co-authored 100 publications receiving 9371 citations. Previous affiliations of John O. Stone include Australian National University & Missouri State University.

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Air pressure and cosmogenic isotope production

TL;DR: In this article, it was shown that the cosmic ray flux increases at higher altitude as air pressure and the shielding effect of the atmosphere decrease, and that altitude-dependent scaling factors are required to compensate for this effect in calculating cosmic ray exposure ages.
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A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements

TL;DR: In this paper, the authors present a single complete and straightforward method that reflects currently accepted practices and is consistent with existing production rate calibration measurements, which is intended to enable geoscientists, who wish to use cosmogenic-nuclide exposure age or erosion rate measurements in their work, to calculate exposure ages and erosion rates; compare previously published exposure ages on a common basis; and evaluate the sensitivity of their results to differences between published production rate scaling schemes.
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Geological calibration of spallation production rates in the CRONUS-Earth project

TL;DR: In this article, the authors describe a calibration procedure developed during the Cosmic-Ray Produced Nuclide Systematics on Earth (CRONUS-Earth) project and its application to an extensive data set that included both new cosmogenic nuclide samples and samples from previously published studies.
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Cosmogenic chlorine-36 from calcium spallation

TL;DR: In this article, the authors measured the spallation rate of calcite at Tabernacle Hill basalt at an altitude of 1445 m and an effective geomagnetic latitude of 40.9 ° and estimated the corresponding rate at sea level and high latitude at 48.8 ± 3.4 atoms (g Ca)−1 a−1.
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Holocene Deglaciation of Marie Byrd Land, West Antarctica

TL;DR: The surface exposure ages of glacial deposits in the Ford Ranges of western Marie Byrd Land indicate continuous thinning of the West Antarctic Ice Sheet by more than 700 meters near the coast throughout the past 10,000 years as discussed by the authors.