Interspatial Data:Meteorite Formation

METEOR COMPOSITION: [1]50% metal/50% silicates [2]IRON:34.63 OXYGEN:29.53% SILICON:15.20% MAGNESIUM:12.70%[potential cause of flame] NICKEL:2.39% SULFUR:1.93%[cause of flame] CALCIUM:1.13% ALUMINUM:1.09% SODIUM/KALIUM/CHROMIUM/COBALT/MANGANESE/PHOSPHORUS/TITANIUM:1%-0.1% Fe[+2] and Fe[+3] are most predominant. Meteorites also contain magnetite[Fe3o4-harness:6.strongly magnetic]Magnetite is also Fe24. hese are potential reactions of a planet before explosion: Fe2+Fe3+3Co2.This is under carbonic tmosheres 3Fe2o3=3Fe2+4o2+OH Fe3+2Co2=Fe3O4++2C Fe[+2]+Fe[+3]+3CO2=Fe3O4+Fe[+2]+CO2 3FeO=Fe3+CO2+CO If heated iron globules enter into a CO2 frozen atmoshere,a planet will explode due to paramagnetic oxygen being magnetically pulled to iron out of the undersurface after the CO2 instantaneously evaporates.CO2 destabilization and instantaneous O2 paramagnetic attraction to the iron would cause an explosion due to ultracold and ultrahot temperature matter concatenating.Magnesium being present in larger quantities would ignite in n oxygen rich atmoshere.Other metals, functioning as catalysts,cause an instantaneous explosive reaction.