Allochem

Allochem is a term introduced by Folk[1] to describe the recognisable "grains" in carbonate rocks.

Examples would include ooids, peloids, oncolites, pellets, fossil or pre-existing carbonate fragments.

Fragments are still termed allochems if they have undergone chemical transformations – for example if an aragonite shell were to dissolve and be later replaced by calcite, the replacement would still be deemed an allochem.

[2] The allochems are typically embedded in a matrix of micrite (lime mud) or sparry calcite.

This sedimentology article is a stub.