The volatility trend of a planetary body is the decrease of its abundances, relative to the CI chondrites and normalised to a refractory element, with decreasing condensation temperature: refractory elements stand in their chondritic proportions, moderately volatile ones are depleted the more the lower their condensation temperature.
书籍暂未推出简体中文版——当前显示英文版。
Earth and Space Sciences · 术语表