Typically this occurs as a result of a marine transgression or regression, or the progressive development of a delta. As the shoreline advances or retreats, a succession of continuous deposits representing different environments (for example beach, shallow water, deeper water) may be left behind. Although each type of deposit (facies) may be continuous over a wide area, its age varies according to the position of the shoreline through time.
An example is the sandy beds near the end of the lower Carboniferous of the west of England, for example the Drybrook sandstone of the Forest of Dean. Deposition of this began much later in the Bristol area than further north.
The detection of diachronous beds can be quite problematic since fossil assemblages tend to migrate geographically with their environment of formation. They are generally revealed by the presence of marker species, fossils which
Diachronous Late-Stage Exhumation across the Western Alpine Arc: Constraints from Apatite Fission-Track Thermochronology between the Pelvoux and Dora-Maira Massifs
Jan 01, 2007; Abstract: We present new apatite fission-track (AFT) data from the central western Alps that confirm the synchronicity and high...