Allochem
Allochem is a term introduced by Folk [1] to describe the recognisable "grains" in carbonate rocks . Any fragment from around 0.5 mm upwards in size may be considered an allochem. 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] Ooids on the surface of a limestone ; Carmel Formation (Middle Jurassic ) of southern Utah, USA. Largest is 1.0 mm in diameter. The allochems are typically embedded in a matrix of micrite (lime mud) or sparry calcite. This article uses material from the Wikipedia article Metasyntactic variable , which is released under the Creative C...