Laboratoire de Géologie de Lyon, ENS Lyon, CNRS and Université Claude Bernard de Lyon, Lyon, France.
Science. 2012 Mar 23;335(6075):1477-80. doi: 10.1126/science.1219509. Epub 2012 Mar 1.
The compositions of Earth materials are strikingly similar to those of enstatite chondrite meteorites in many isotope systems. Although this suggests that Earth largely accreted from enstatite chondrites, definitive proof of this model has been lacking. By comparing the silicon (Si) isotope signatures of several extraterrestrial materials with terrestrial samples, we show that they cannot be explained by core-formation scenarios involving a bulk Earth of enstatite chondrite composition. Si isotope similarities between the bulk silicate Earth and the Moon preclude the existence of a hidden reservoir in the lower mantle, a necessary condition of the enstatite chondrite model, and require an equilibrium process after the Moon-forming impact. A three-end-member chondritic mixing model for Earth reconciles the Si isotope similarities between enstatite chondrites and Earth.
地球物质的组成在许多同位素体系中与顽辉石球粒陨石非常相似。尽管这表明地球主要由顽辉石球粒陨石吸积而成,但这一模型一直缺乏确凿的证据。通过比较几种外星物质和地球样本的硅(Si)同位素特征,我们表明它们不能用涉及顽辉石球粒陨石组成的整体地球的核形成情景来解释。地幔下部存在一个隐藏的储层是顽辉石球粒陨石模型的必要条件,而整个硅酸盐地球和月球之间的 Si 同位素相似性排除了这种可能性,这就需要在月球形成的撞击之后发生一个平衡过程。一个三端元球粒陨石混合模型可以协调顽辉石球粒陨石和地球之间的 Si 同位素相似性。