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Research Article| January 01, 2002 Origin of Noble Gases in the Terrestrial Planets Robert O. Pepin; Robert O. Pepin School of Physics and Astronomy, University of Minnesota, 116 Church Street S.E., Minneapolis, Minnesota 55455, pepin001@tc.umn.edu Search for other works by this author on: GSW Google Scholar Donald Porcelli Donald Porcelli Department of Earth Science, University of Oxford, Parks Road, Oxford, OX1 3PR, United Kingdom Search for other works by this author on: GSW Google Scholar Author and Article Information Robert O. Pepin School of Physics and Astronomy, University of Minnesota, 116 Church Street S.E., Minneapolis, Minnesota 55455, pepin001@tc.umn.edu Donald Porcelli Department of Earth Science, University of Oxford, Parks Road, Oxford, OX1 3PR, United Kingdom Publisher: Mineralogical Society of America First Online: 13 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2002) 47 (1): 191–246. https://doi.org/10.2138/rmg.2002.47.7 Article history First Online: 13 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Robert O. Pepin, Donald Porcelli; Origin of Noble Gases in the Terrestrial Planets. Reviews in Mineralogy and Geochemistry 2002;; 47 (1): 191–246. doi: https://doi.org/10.2138/rmg.2002.47.7 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 Identifying the mechanisms that drove the evolution of planetary volatiles from primordial to present-day compositions is one of the classic challenges in the planetary sciences. The field bristles with models of one type or another, but none are without difficulties. Efforts to understand the histories of volatile species in the atmospheres and interiors of the terrestrial planets have concentrated on their noble gases, free of the entanglements of chemical interaction, as evolutionary tracers. The elemental and isotopic compositions of these minor constituents are rich in clues to the chemical characteristics of their source reservoirs, the physics of their evolution, and... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Published in: Reviews in Mineralogy and Geochemistry
Volume 47, Issue 1, pp. 191-246