The stone in the stone iron meteorite is a stone. Iron is iron. The two are mixed. It is an irregular mixture of stone and pure iron, not completely integrated, but a cry of completely integrated compounds. Iron ore is almost a single or multiple iron-containing compounds. Iron meteorites are almost pure iron and nickel, but also contain a small amount of meteorite iron, olivine, graphite, iron phosphate, giant chromite, Alkki iron, chromite and so on, which is also the difference between iron. An important symbol of iron. Iron meteorites are divided into various nickel-free hexagons, with medium-nickel fine lines, such as Flame Mountain, high-nickel creative sputum, and then high-nickel no texture. The amount of nickel gradually transits. The common M-iron and G-events belong to octahedron. For unknown types of iron meteorites, friends are advised not to do anything in general. Because it's acid-washed, it's a real meteorite, and it doesn't necessarily run out in the ditch. There is a special species that few people can identify. To say the least, even octahedral weapons are rarely obtained, but it is right to destroy the baby. You must understand, you can't tell, you must understand, you can't tell solidification.

The gold stage of iron meteorites is closely related to nickel content. The nickel content is less than 6%, and it is dominated by iron stone, which is hexagonal. No vision debut structure; Niobite with increased nickel content has a structure of Sens station, in which the nickel-iron lines are crossed and parallel, with 8 vertical planes. With the increase of nickel content, the texture began to be rough, about 20%, and the ripples became quite good. Need to look at the very fine pattern again under the microscope; Then the content of nickel increased, and it was completely dominated by nickel stone, which was no longer an eighth size. We are actually talking about a kind of crystal growth. At almost constant space temperature (why it is constant), iron and nickel expand in different directions, forming an octave. Nickel is too high. Or too low, it is not a test terminal structure. There must be two.

The basic differences between iron meteorites and iron ore and stone iron meteorites and the introduction of iron meteorites and iron ore and stone iron meteorites show that the subway aperture is mainly octahedron. The nickel content of iron meteorites in Huoyan Mountain of Xinjiang is about 20%, so the density is quite good and the crystal texture is very beautiful. If the nickel content is high, it can't be seen.