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  • . lower initial gradient. Fig. 1. Use of estimated fluvial palaeotopography in
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  • of a Neoproterozoic basin (Grey & Blake,. 1999; Grey, pers. Comm., 2001). J.F.
  • No obvious r 2004 Blackwell Publishing Ltd, Basin Research, 16, 507^534
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  • MTCs, mass transport complexes. r 2007 The Authors. Journal compilation r
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  • Both steady-state and disequilibrium landscapes are con- alluvial reaches above
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  • Sep 28, 2011 . Basin Research, 23 (5). pp. 571-590. ISSN 0950-091X http://resolver.caltech.edu/
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  • that the Cook Strait Canyon system is unlikely to have been an abundant supplier
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  • . the basin formed by eastward tilting phological criteria in a neotectonic setting (
  • Monash University > Research at Monash > Researcher profiles . Canadian
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  • G(x,t) is first parameterized by zontal and vertical velocity fields, u(x,t) and v(x,z,t),.
  • basic and applied ecology (ONLINE) Elsevier basin research (ONLINE) wiley-
  • many. Basin Research (2006) 18, 145–170, doi: 10.1111/j.1365-2117.2006.
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  • TheUpper Cretaceous basin ll is divided into ve megasequences bounded by . .
  • Oct 14, 2010 . Basin Research, 14 (4). pp. 531-542. ISSN 0950-091X . Published Version: http:
  • As recently as the early 1900s, averaged over 103 years, the Alsek River may be
  • position of the `Capricorn Plate' as inferred by Royer & Gordon (1997). D.
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