Ore Deposits Formed by Regional Metamorphism
Learn about metamorphic ore deposits formed by regional metamorphism, including the formation of valuable non-metallic ores like graphite, talc, garnet, asbestos, and more. Explore how metamorphism alters mineralogy, texture, and structure of ores, with examples such as graphite origin and metamorphic graphite genesis.
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Presentation Transcript
4- Ore deposits formed by regional metamorphism (Metamorphic ore deposits) Metamorphic ores : Are ores whose minerals are formed directly by metamorphism. Many valuable non-metallic ore deposits (graphite, talc, garnet, asbestos, sillimanite, serpentine) formed as a product of metamorphism because of recrystallization and recombination of rock forming minerals. No new constituents are introduced except for water and Co2
Metamorphosed ores: Are preexisting ores that suffer metamorphism after their formation. Metamorphism alters the `mineralogy, texture and structure of the ores. Agencies of metamorphism: heat, pressure, solution and time. Example : Graphite ore deposits
Graphite originates by: 1. Regional metamorphism 2. Crystallization of igneous rocks (it occurs in granite, syenite and basalt). 3. Contact metamorphism metamorphic silicates in limestone adjacent to igneous intrusion. It results from carbon compound bearing solution given off from the magma. 4. Hydrothermal (as vein deposits in pegmatite). It results from carbon compound bearing solution given off from the magma. (occurs in contact
Genesis of metamorphic graphite Two Views: 1- The graphite is altered organic matter present in the sediments : The black carbonaceous limestone altered by metamorphism to white marble and disseminated graphite. The carbonaceous matter is originally hydrocarbons that may be either broken up or reduced to graphite or it converted to CO and CO2that will be reduced to graphite. 2- The carbonate breaks down yielding their Ca, Mg and Fe to form silicates and releasing CO and CO2which in turn becomes reduced to form graphite. CO2+ 2H2 C + 2H2O 2CO C + CO2
