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.
Limestone is made of calcium carbonate (CaCO3).
limestone, chalk and marble.
Limestone, calcite chalk and marble.
chalk
When acid rain reacts with the carbonate rocks, carbon dioxide is usually released into the air.
No. Mainly rocks with a high content of iron. Rocks such as silica or calcium carbonate are not.
The reaction of carbonic acid in rain and groundwater with the carbonate rock.
by means of plants
Although the carbonic acid contained in rainwater aid in the erosion of all rocks, most susceptible are the carbonate rocks such as limestone.
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.
There is carbon dioxide in the sea and animals die and falkl to tyhe sea bed and create carbonate in rocks
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)
When acid rain reacts with the carbonate rocks, carbon dioxide is usually released into the air.
carbonate containing rocks
Carbonate rocks.
No. Mainly rocks with a high content of iron. Rocks such as silica or calcium carbonate are not.
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
The reaction of carbonic acid in rain and groundwater with the carbonate rock.
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