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References 
Deflation and dust offshore West Africa: in drylands, many fine-grained deposits developed during wet climate phases, such as lacustrine deposits, are deflated away during arid periods.
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.
Savannah is not just wide grassy plains as portrayed by Hollywood in Out of Africa, and many ancient dryland successions probably formed in tropical savannah settings.
Regions of extensive rift basin development may have basins dominated by local basin margin (transverse) alluvial systems and lithofacies not by through-flowing axial rivers.
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.
