* Limestone: Composed primarily of calcium carbonate (CaCO3), limestone is formed by the precipitation of calcite from seawater. It is a common rock found in marine environments, often formed from the accumulation of the shells and skeletons of marine organisms, such as corals, mollusks, and algae.

* Dolostone: Similar to limestone, dolostone is also composed of calcium carbonate, but it contains a significant amount of magnesium (Mg). Dolostone is formed when magnesium ions replace some of the calcium ions in calcite during the precipitation process. It is also commonly found in marine environments and can be associated with limestone formations.

* Chert: Chert is a fine-grained sedimentary rock primarily composed of microcrystalline quartz (SiO2). It is formed by the precipitation of silica from seawater, often in the form of microscopic organisms called diatoms and radiolarians. Chert is commonly found in association with carbonate rocks, such as limestone and dolostone, and can be formed through the replacement of carbonate minerals by silica.

* Evaporites: Evaporites are sedimentary rocks formed by the precipitation of minerals from concentrated brines or evaporating seawater. They include various types of rocks, such as gypsum, anhydrite, halite (rock salt), and potash salts. Evaporites are formed when seawater is trapped in shallow basins and subjected to intense evaporation, leading to the concentration and crystallization of dissolved salts.