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References 
Large and small rivers can co-exist in the same valley system: have you thought about including these in your reservoir models? The little rivers on the left would be thought big if not next to the 15km wide Jamuna R. here.
Better ways to select modern analogues, using climate and geomorphological relationships ...
New website of interest: SEPM Sequence Stratigraphy (STRATA) site by Chris Kendall ...
Debris-flows in action, if you want a thrill ...…
Phase-1 PhD studies incorporated …
Be more precise with your climate zones …
Pictorial lithofacies atlas beginning to be populated - try desiccation cracks to see full potential
Welcome to the AUDRI website
This is the completely rewritten version of the website: new layout, all sections rewritten to improve clarity, many more images, greatly improved navigation, new content. A primary aim is to make more obvious what is inside - so each major section has a much more detailed index page, and it is easier to jump into sub-sections.
Look out for the new Topic Thread navigation (top left and top right) to guide you through longer sections.
Look in Reservoirs and Analogues section for a guide to conceptual and numerical reservoir modelling.
Tell us what you think, share ideas or ask questions, through the Feedback section.
A drying climate change will leave lake deltas stranded in the landscape and looking at first sight like fluvial fans
Wind-blown dust can add large amounts of clay to sediment that might have been deposited free of clay, confusing environmental interpretation
Models for meandering river reservoirs usually over-estimate sand-body connectivity because it is assumed such rivers produce shoe-string ribbons of sand that are well-connected along the valley - this is rarely true.
