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Featheredge pinchouts of successions composed of sheetlike sandstone beds, such as turbidite lobes or shorederived midshelf tempestites are extremely difficult to recognize and model. Both turbidites and tempestites are expected to pinch out seawards, but their actual thinning rates and pinchout geometries are littleknown and unpredictable. In the present pilot study, more than 3750 closely spaced measurements of the lateral thickness changes in 146 turbidite and tempestite beds have been collected over lateral outcrop distances of up to 640 m. The datasets show that both turbidites and tempestites have a lognormal thickness frequency distribution. Assuming the bed segments measured in outcrop sections represent downflowthinning segments of unconfined turbidites and tempestites, their thinning rates can be stacked together according to the local bedthickness ranges to represent the pinchout geometry of a whole single bed. The rangerelated trend equations allow the pinchout distance of every bed in a turbiditic or tempesitic succession encountered in a well to be predicted and the net spatial pinchout of a given bed succession to be modelled.
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