Sandstones with abundant lithics, feldspars, or [[chert]] have less occlusion of [[porosity]] by quartz overgrowths and more secondary porosity through dissolution of less stable grains. The ratio of quartz to [[Ductility|ductile]] grains is key to compaction porosity loss. | Sandstones with abundant lithics, feldspars, or [[chert]] have less occlusion of [[porosity]] by quartz overgrowths and more secondary porosity through dissolution of less stable grains. The ratio of quartz to [[Ductility|ductile]] grains is key to compaction porosity loss. |