Under the Dunham classification (Dunham, 1962[1]) system of limestones, a packstone is defined as a grain-supported carbonate rock that contains 1% or more mud-grade fraction. This definition has been clarified by Lokier and Al Junaibi (2016)[2]asa carbonate-dominated lithology containing carbonate mud (<63 μm) in a fabric supported by a sand grade (63 μm to 2 mm) grain-size fraction and where less than 10% of the volume consists of grains >2 mm.
A study of the adoption and use of carbonate classification systems by Lokier and Al Junaibi (2016)[2] identified three common problems encountered when describing a packstone:
