Anomalous magnesium isotopes in meteorites
1986 年 20 巻 6 号 p. 311-316
詳細
1986 年 20 巻 6 号 p. 311-316
The origin of the isotopically anomalous magnesium components reported to have been discovered in high-temperature mineral inclusions of carbonaceous chondrites can be attributed to the alterations of the isotopic composition caused primarily by high-energy proton reactions, which occurred within the solar system when the Sun was in its T-Tauri phase.
