Because the crystal lattice of dolomite is more compact than calcite, this chemical transformation frequently generates significant secondary intercrystalline porosity, making dolostones premier reservoirs for groundwater and hydrocarbons. Geochemical Archives and Earth History

Shallow-water carbonates are robust indicators of tropical to subtropical, clear water conditions.

Focuses on the depositional texture, distinguishing between grain-supported and mud-supported fabrics (e.g., mudstone, wackestone, packstone, grainstone, boundstone).