Abstract

A unique occurrence of lithified, fluvial armored mud balls has been found in the Lower Jurassic Turners Falls Sandstone of north-central Massachusetts. The long axes of the 55 examples range from 2.5 to 30 cm, which agrees with previous studies of modern armored mud balls. Their triaxial ellipsoidal shapes differ from the usual spheroid shapes of modern examples. It is inferred that they formed quickly, after only a few hundred meters of transport in a distal fan environment.

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