Arid

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Tracking the Be-10-Al-26 source-area signal in sediment-routing systems of arid central Australia 期刊论文
发表期刊: EARTH SURFACE DYNAMICS. 出版年: 2018, 卷号: 6, 期号: 2, 页码: 329-349
作者:  Struck, Martin;  Jansen, John D.;  Fujioka, Toshiyuki;  Codilean, Alexandru T.;  Fink, David;  Fulop, Reka-Hajnalka;  Wilcken, Klaus M.;  Price, David M.;  Kotevski, Steven;  Fifield, L. Keith;  Chappell, John
收藏  |  浏览/下载:17/0  |  提交时间:2019/11/29
Soil production and transport on postorogenic desert hillslopes quantified with Be-10 and Al-26 期刊论文
发表期刊: GEOLOGICAL SOCIETY OF AMERICA BULLETIN. 出版年: 2018, 卷号: 130, 期号: 5-6, 页码: 1017-1040
作者:  Struck, Martin;  Jansen, John D.;  Fujioka, Toshiyuki;  Codilean, Alexandru T.;  Fink, David;  Egholm, David L.;  Fulop, Reka-Hajnalka;  Wilcken, Klaus M.;  Kotevski, Steven
收藏  |  浏览/下载:16/0  |  提交时间:2019/11/29
Discordance between cosmogenic nuclide concentrations in amalgamated sands and individual fluvial pebbles in an arid zone catchment 期刊论文
发表期刊: QUATERNARY GEOCHRONOLOGY. 出版年: 2014, 卷号: 19, 页码: 173-180
作者:  Codilean, Alexandru T.;  Fenton, Cassandra R.;  Fabel, Derek;  Bishop, Paul;  Xu, Sheng
Adobe PDF(1205Kb)  |  收藏  |  浏览/下载:17/6  |  提交时间:2019/11/29
Beryllium-10  Aluminium-26  Neon-21  Cosmogenic nuclide  Grain size bias  Namibia  
Cosmogenic Ne-21 analysis of individual detrital grains: Opportunities and limitations 期刊论文
发表期刊: EARTH SURFACE PROCESSES AND LANDFORMS. 出版年: 2010, 卷号: 35, 期号: 1, 页码: 16-27
作者:  Codilean, Alexandru T.;  Bishop, Paul;  Hoey, Trevor B.;  Stuart, Finlay M.;  Fabel, Derek
收藏  |  浏览/下载:15/0  |  提交时间:2019/11/29
cosmogenic nuclide analysis  landscape evolution  numerical modelling  sediment provenance  Namibia  
Single-grain cosmogenic Ne-21 concentrations in fluvial sediments reveal spatially variable erosion rates 期刊论文
发表期刊: GEOLOGY. 出版年: 2008, 卷号: 36, 期号: 2, 页码: 159-162
作者:  Codilean, Alexandru T.;  Bishop, Paul;  Stuart, Finlay M.;  Hoey, Trevor B.;  Fabel, Derek;  Freeman, Stewart P. H. T.
收藏  |  浏览/下载:8/0  |  提交时间:2019/11/28
Ne-21  Be-10  cosmogenic nuclides  denudation rates  slope dependence  landscape evolution