EARLY POST-DEPOSITIONAL BEDDING-PLANE-PARALLEL MELANGES CREATED BY SHEAR AND LIQUEFACTION: A COMMON BUT LARGELY MISINTERPRETED ORGANIC-RICH MUDROCK FACIES
When noted at all, "dead horse" mélanges have been interpreted as depositional units such as turbidites, rip-up clasts indicating subaerial exposure, slumps, or seismites, but we interpret them as “early” shear and dewatering-related units that did not have a free surface at the time of deformation. These are very common; in lacustrine sequences of the Triassic-Jurassic of the eastern US, nearly every sedimentary cycle with a dark gray to black mudstone has such a layer, amounting to hundreds of beds. Similar beds are abundant in the Eocene Green River Fm and are found in many other organic-rich, laminated mudstone sequences.
Assuming these mélanges are depositional leads to very serious mistakes in environmental interpretation. Moreover, because they formed post-depositionally, between pre-existing beds, and their formation was controlled by a combination of specific rheology at unknown depths and pressures (with or without specific triggers) each bed cannot be treated as resulting from a specific event, and a stratigraphy of sequential beds cannot be interpreted as a history of events. Given their virtual lack of recognition, the effects of these mélanges on diagenesis or fluid and gas generation and migration are wholly unknown.