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• W2019957896 abstract "Research Article| May 01, 2007 Cantor set model of eolian dust deposits on desert alluvial fan terraces Jon D. Pelletier Jon D. Pelletier 1Department of Geosciences, University of Arizona, Gould-Simpson Building, 1040 East Fourth Street, Tucson, Arizona 85721–0077, USA Search for other works by this author on: GSW Google Scholar Geology (2007) 35 (5): 439–442. https://doi.org/10.1130/G23367A.1 Article history received: 15 Sep 2006 rev-recd: 21 Dec 2006 accepted: 28 Dec 2006 first online: 09 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 Jon D. Pelletier; Cantor set model of eolian dust deposits on desert alluvial fan terraces. Geology 2007;; 35 (5): 439–442. doi: https://doi.org/10.1130/G23367A.1 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 SocietyGeology Search Advanced Search Abstract Available data show that eolian dust accumulation rates on desert alluvial fan terraces are often inversely proportional to the square root of the terrace age for a given area. This temporal scaling is similar to that observed in fluvial and marine stratigraphic sequences in which a fractal distribution of hiatuses occurs (i.e., a Cantor set). Eolian dust accumulation on alluvial fan terraces is controlled by regional climatic influences on dust deposition (e.g., dessication of pluvial lakes in the early Holocene) and local surface characteristics (e.g., vegetation and pavement coverage) that control dust preservation. In order to interpret the observed scaling in terms of these relative influences I consider two end-member models: (1) a deterministic model in which dust deposition is controlled by cyclical climatic changes (i.e., glacial-interglacial cycles) and in which no erosion occurs, and (2) a stochastic model in which erosion and deposition take place with equal probability and magnitude during each time step (i.e., a bounded random walk). The observed temporal scaling is most consistent with the bounded random walk model, suggesting that long-term eolian dust accumulation is predominantly controlled by episodic changes in vegetation and pavement coverage over time and that eolian dust deposits are strongly punctuated by episodes of erosional reworking at a wide range of temporal scales. 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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• W2019957896 title "Cantor set model of eolian dust deposits on desert alluvial fan terraces" @default.
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