What is carbonatite?

Carbonacy is a form of volcanic rock, which usually has different minerals. Similar to carbonates that usually occur in the ocean, can often be seen in the center-contact seismic zones, such as Great Rift Valley in Africa or the state of Nevada in the United States. Minerals such as iron, barium, calcite and dolomites are often seen in carbonatite. It sometimes contains a small amount of uranium, titanium or phosphorus.

Lava, which flows to the surface or molten rock that penetrates into the materials underground can form carbonacy. Structures in the ground, such as dams or window sills, which usually solidify when molten rock passes through older layers of rocks, often also contain carbonatite. The volcanic rocks were once considered rare, but research has shown that it is often formed and then worn once in contact with the atmosphere. Contuvs can be carbotite. These usually melt at a relatively lowsiring temperatures or become a powder material that blows through the wind or retreats with rain or running water.

mining operations are often performed in open pits to get to carbotatity. Minerals contained in the rock and others, sometimes found in the surroundings, are often considered desirable in many industries. In addition to the health risks of dust, acid or some metals, deposits may include radioactive compounds such as uranium or thorium. Chemicals and waste products that are often used in the process in this process can collect waste for waste or leakage into groundwater and sometimes also become health risks.

It is assumed that some carbonatite deposits have been formed relatively recently, but can also be associated with most of the Earth's history. They are usually seen in different types of landscapes, from mountainous terrain to zemklobouk is rEltatively flat. This rock deposition, which is also located in a country where there are no mistakes or other types of shear zones, can be located by monitoring the calculations rich in calcite, which move in running groundwater.

magnetic and gravitational differences can be detected in a rock that contains carbonatite deposits. In addition to Africa and the United States, these volcanic rocks often occur in Canada, Brazil, Russia and India. They are generally associated with specific rock formations in Australia, Norway and Spain. Active carbonite volcanoes are rare, while older sometimes occur in geologically active, medium continental areas.