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Rates and Timing of Earth Surface Processes From In Situ-Produced Cosmogenic Be-10

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2002

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Research Article| January 01, 2002 Rates and Timing of Earth Surface Processes From In Situ-Produced Cosmogenic Be-10 Paul R. Bierman; Paul R. Bierman Geology Department and School of Natural Resources University of Vermont, Burlington, Vermont 05405, pbierman@zoo.uvm.edu Search for other works by this author on: GSW Google Scholar Marc W. Caffee; Marc W. Caffee Center for Accelerator Mass Spectrometry Lawrence Livermore National Laboratory Livermore, California 94550, Now at: PRIME Lab, Purdue University, West Lafayette, Indiana 47907 Search for other works by this author on: GSW Google Scholar P. Thompson Davis; P. Thompson Davis Department of Natural Science, Bentley College Waltham, Massachusetts 02152 Search for other works by this author on: GSW Google Scholar Kim Marsella; Kim Marsella Geology Department, Skidmore College Saratoga Springs, New York 12866 Search for other works by this author on: GSW Google Scholar Milan Pavich; Milan Pavich National Center, U S Geological Survey Reston, Virginia 22092 Search for other works by this author on: GSW Google Scholar Patrick Colgan; Patrick Colgan Department of Geology, Northeastern University Boston, Massachusetts 02115 Search for other works by this author on: GSW Google Scholar David Mickelson; David Mickelson Department of Geology & Geophysics, University of Wisconsin Madison, Wisconsin 53706 Search for other works by this author on: GSW Google Scholar Jennifer Larsen Jennifer Larsen Geology Department, University of Vermont Burlington, Vermont 05405 Search for other works by this author on: GSW Google Scholar Author and Article Information Paul R. Bierman Geology Department and School of Natural Resources University of Vermont, Burlington, Vermont 05405, pbierman@zoo.uvm.edu Marc W. Caffee Center for Accelerator Mass Spectrometry Lawrence Livermore National Laboratory Livermore, California 94550, Now at: PRIME Lab, Purdue University, West Lafayette, Indiana 47907 P. Thompson Davis Department of Natural Science, Bentley College Waltham, Massachusetts 02152 Kim Marsella Geology Department, Skidmore College Saratoga Springs, New York 12866 Milan Pavich National Center, U S Geological Survey Reston, Virginia 22092 Patrick Colgan Department of Geology, Northeastern University Boston, Massachusetts 02115 David Mickelson Department of Geology & Geophysics, University of Wisconsin Madison, Wisconsin 53706 Jennifer Larsen Geology Department, University of Vermont Burlington, Vermont 05405 Publisher: Mineralogical Society of America First Online: 14 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2002) 50 (1): 147–205. https://doi.org/10.2138/rmg.2002.50.4 Article history First Online: 14 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Paul R. Bierman, Marc W. Caffee, P. Thompson Davis, Kim Marsella, Milan Pavich, Patrick Colgan, David Mickelson, Jennifer Larsen; Rates and Timing of Earth Surface Processes From In Situ-Produced Cosmogenic Be-10. Reviews in Mineralogy and Geochemistry 2002;; 50 (1): 147–205. doi: https://doi.org/10.2138/rmg.2002.50.4 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search Beryllium-10 is the longest-lived of the seven known unstable isotopes of Be; it results mostly from the interaction of cosmic radiation, primarily neutrons, with a variety of target atoms by spallation, the splitting of nuclei (Lal 1988). It can also be produced at very low levels by radio-disintegration of U and Th (Sharma and Middleton 1989). Although all radioactive Be isotopes are produced in the atmosphere via cosmic-ray reactions (Arnold 1956; Lal and Peters 1967; Morris et al., Chapter 5, this volume), in this paper, we are most interested in 10Be produced... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

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