What Is an Iron Meteorite?
Meteorite, iron meteorite, meteorite whose main ingredient is iron and nickel.
- An iron meteorite with an Ni content of about 6 to 14%. It has an image composed of grains of ferrite and nickel grains. This image is called
- Two classifications were used. Earlier structural classifications were based on percentages or Weidmannian patterns, which can be evaluated from the cross-stripes that appear on the polished surface after etching with acid. This classification is linked to the relative abundance of iron and nickel and is classified as [2]
- Iron-nickel alloys were used by many cultures to make tools and weapons, for example, parts of the Cape York meteorite used by the Inuit [3]
Iron meteorite China
- China's largest iron meteorite
- The third largest in the world in 1898,
- Xinjiang iron meteorite (4 photos)
- Historically, a large meteorite rain has occurred in Qinghe County. No matter the scattered area, scale and number of meteorites, they are all the highest in the world. The meteorite is currently deposited in the Xinjiang Geological and Mineral Museum. It is now on display in the Xinjiang Exhibition Center in China.
- China's second largest iron meteorite
- Also called Lingshi, in the Luzu Temple outside the north gate of the old city of Lingshi County.
- Iron meteorite in Lingshi County-China's second largest iron meteorite (4 photos)
- China's third largest iron meteorite
- In 2000, archaeologists from the Xinjiang Museum also found iron meteorite clusters with a scattered area of several square kilometers in a ravine in the northwest of Qinghe County, northern Xinjiang. According to the composition, density and volume of the meteorite, it is presumed that some of the meteorite weighed more than 100 tons. The meteorite group discovered this time is also located in the Altai region of Xinjiang, and the number reaches thousands.
Iron meteorite USA
- On July 18, 2014,
- The iron meteorite seems like a huge burning object with a surface filled with angular cavity structures. Scientists believe that this may be formed by erosion of metal crystals on the edge of the rock. Another possible explanation is that these hollow cavity structures and olivine Specifically, this kind of material can be found in rare stone meteorites, and the formation process of the latter is more complicated. Generally, scientists think that it is formed on the boundary layer near the planet's core and mantle. Obviously, the stone meteorite is a relatively rare material. . [4]