1 Possible forms of nebular condensation The condensation can include two processes: gas-solid and gas-liquid-solid condensations. Because nebular condensation occurred with temperature descending slowly, the forms of...1 Possible forms of nebular condensation The condensation can include two processes: gas-solid and gas-liquid-solid condensations. Because nebular condensation occurred with temperature descending slowly, the forms of solar nebular condensation is dependent on the relationship between the pressure of nebular and‘triple point’ of nebular matter. Based on vapor-condensation experiments of main silicate minerals in chondrites, Kushiro indicated that the pressure range展开更多
The study of Mg isotopes has been carried out for about 40 years since 1970 s. With analytical progress, the study is not only limited to the excess of ^26Mg due to decay of short-lived ^26Al in primitive meteorites, ...The study of Mg isotopes has been carried out for about 40 years since 1970 s. With analytical progress, the study is not only limited to the excess of ^26Mg due to decay of short-lived ^26Al in primitive meteorites, also extended to mass-dependent fractionation of Mg isotopes in meteorites and terrestrial rocks. This paper reviews recent development in Mg isotope researches.展开更多
基金the National Natural Science Foundation of China.
文摘1 Possible forms of nebular condensation The condensation can include two processes: gas-solid and gas-liquid-solid condensations. Because nebular condensation occurred with temperature descending slowly, the forms of solar nebular condensation is dependent on the relationship between the pressure of nebular and‘triple point’ of nebular matter. Based on vapor-condensation experiments of main silicate minerals in chondrites, Kushiro indicated that the pressure range
基金supported by the Pilot Project of Knowledge Innovation Program of the Chinese Academy of Sciences(kzcx2-yw-Q08)the Natural Science Foundation of China(Grants 40873054)
文摘The study of Mg isotopes has been carried out for about 40 years since 1970 s. With analytical progress, the study is not only limited to the excess of ^26Mg due to decay of short-lived ^26Al in primitive meteorites, also extended to mass-dependent fractionation of Mg isotopes in meteorites and terrestrial rocks. This paper reviews recent development in Mg isotope researches.
