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- W2059264839 abstract "Research Article| January 01, 2005 Quantitative Constraints on the Rate of Landform Evolution Derived from Low-Temperature Thermochronology Jean Braun Jean Braun Research School of Earth Sciences, The Australian National University, Canberra ACT 0200, Australia, (Now at Géosciences-Rennes, Université de Rennes 1, Rennes 35042, France) Jean.Braun@univ-rennes1.fr Search for other works by this author on: GSW Google Scholar Author and Article Information Jean Braun Research School of Earth Sciences, The Australian National University, Canberra ACT 0200, Australia, (Now at Géosciences-Rennes, Université de Rennes 1, Rennes 35042, France) Jean.Braun@univ-rennes1.fr Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2005) 58 (1): 351–374. https://doi.org/10.2138/rmg.2005.58.13 Article history First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Jean Braun; Quantitative Constraints on the Rate of Landform Evolution Derived from Low-Temperature Thermochronology. Reviews in Mineralogy and Geochemistry 2005;; 58 (1): 351–374. doi: https://doi.org/10.2138/rmg.2005.58.13 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 In recent years, the nature of the complex interactions between the solid earth and the overlying atmosphere has been the subject of much debate (England and Molnar 1990; Whipple et al. 1999; Braun et al. 1999). Does erosion play an important role in the dynamics of mountain building? Is there a strong feedback into the balance of forces at the crustal scale from mass transport by erosional and depositional processes at the Earth’s surface? Or does erosion passively react to changes in the Earth’s surface topography to shape mountains with tectonic forces, originating in the underlying... You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W2059264839 date "2005-01-01" @default.
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- W2059264839 title "Quantitative Constraints on the Rate of Landform Evolution Derived from Low-Temperature Thermochronology" @default.
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