Sedimentary rocks are usually divided into: siliciclastic rocks and carbonate rocks. Siliciclastics are usually composed of the weathering products of older rocks carried and delivered to a basin of deposition by rivers. Carbonate rock, however, are generally composed of carbonate minerals (e.g. Calcite, Dolomite, Anhydrite..) these minerals form either biologically (as skeletons of sea organisms such as foraminifera, rudists and corals) or chemically by sea water. The most famous carbonate rock is probably Limestone, other rocks include: Dolostone (aka Dolomite) and evaporites; interesting to note that Marble is metamorphosed limestone.
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∙ 12y agoLimestone and dolomite are common rocks that contain carbonate minerals. These rocks form primarily from the accumulation of calcite or aragonite for limestone, and dolomite for dolomite, often from the remains of marine organisms.
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∙ 14y agoLimestone is made of calcium carbonate (CaCO3).
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∙ 14y agoWiki User
∙ 15y agolimestone, chalk and marble.
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∙ 13y agoLimestone, calcite chalk and marble.
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∙ 14y agochalk
The chemical formula of marl rocks is CaCO3 (calcium carbonate). Marl is a type of sedimentary rock composed of varying proportions of clay and calcium carbonate.
Carbonate rocks, like limestone, can release carbon dioxide when they break down or weather. This process, known as chemical weathering, occurs when carbonic acid in water reacts with the minerals in the rocks, leading to the release of carbon dioxide into the air.
Carbonate weathering is the process by which rocks containing carbonate minerals (such as calcite) are broken down and dissolved due to exposure to carbon dioxide and water. This process can alter the rocks' chemical composition and form new minerals. Carbonate weathering plays a significant role in the carbon cycle and can affect the acidity of soil and water.
Carbon dioxide is released from carbonate rocks into the atmosphere through processes such as weathering, dissolution, and metamorphism. When carbonate rocks are exposed to water or acidic conditions, they break down and release carbon dioxide as a byproduct. This released carbon dioxide can then be released into the atmosphere through various pathways.
Most carbonate rocks, such as limestone and dolomite, are formed through the accumulation and cementation of calcareous marine organisms like corals, mollusks, and algae. These organisms produce calcium carbonate shells and skeletons that build up over time to create carbonate rock formations. Other processes, like precipitation from seawater or chemical reactions in caves, can also contribute to the formation of carbonate rocks.
Carbon dioxide can get locked in carbonate rocks through processes such as weathering of rocks containing carbonates, which leads to the formation of bicarbonate ions that eventually get precipitated as carbonate minerals (e.g., calcite) in rocks. Over time, this process sequesters CO2 in the form of carbonate minerals in the rocks.
There are two effects of carbonate rocks to the global climate. The two effects of carbonate rocks to the global climate are dissolution and deposition.
A. E. Adams has written: 'Atlas of sedimentary rocks under the microscope' -- subject(s): Atlases, Rocks, Sedimentary, Sedimentary Rocks 'A color atlas of carbonate sediments and rocks under the microscope' -- subject(s): Carbonate Rocks, Pictorial works, Rocks, Carbonate, Thin sections (Geology)
carbonate containing rocks
Carbonate rocks.
Limestone, chalk, and marble are examples of rocks that are natural sources of calcium carbonate. These rocks are formed from the accumulation of calcium carbonate minerals over time, which can be used for various purposes including in construction, agriculture, and industry.
Calcium carbonate is a major component of sedimentary rocks such as limestone, chalk, and marble. These rocks form from the accumulation of marine organisms' shells, coral reefs, and precipitated calcite minerals.
C.H Moore has written: 'Carbonate reservoirs : porosity evolution and diagenesis in a sequence stratigraphic framework / Clyde H. Moore' -- subject(s): Carbonate Rocks, Diagenesis, Rocks, Carbonate
Carbonate minerals can form in rocks through the deposition of calcium carbonate (CaCO3) from marine organisms like shells and coral. It can also be introduced through chemical processes, where carbon dioxide combines with minerals in the presence of water to form carbonates.
Terence P. Scoffin has written: 'An introduction to carbonate sediments and rocks' -- subject(s): Carbonate Rocks, Carbonates, Sediments (Geology)
Richard David Harvey has written: 'Lake marls, chalks, and other carbonate rocks with high dissolution rates in SO2-scrubbing liquors' -- subject(s): Marl, Chalk, Carbonate Rocks 'Thermal expansion of certain Illinois limestones and dolomites' -- subject(s): Limestone, Dolomite 'Petrographic properties of carbonate rocks related to their sorption of sulfur dioxide' -- subject(s): Carbonate Rocks
Mark Vernon Mauritsen has written: 'Studies of diagenesis of bermuda limestones' -- subject(s): Carbonate Rocks, Diagenesis, Limestone, Rocks, Carbonate