Institute of Geophysics and Planetary Physics, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA.
Science. 2010 Apr 23;328(5977):483-6. doi: 10.1126/science.1184741. Epub 2010 Feb 25.
We measured the 26Al-26Mg isotope systematics of a approximately 5-micrometer refractory particle, Coki, returned from comet 81P/Wild 2 in order to relate the time scales of formation of cometary inclusions to their meteoritic counterparts. The data show no evidence of radiogenic 26Mg and define an upper limit to the abundance of 26Al at the time of particle formation: 26Al/27Al < 1 x 10(-5). The absence of 26Al indicates that Coki formed >1.7 million years after the oldest solids in the solar system, calcium- and aluminum-rich inclusions (CAIs). The data suggest that high-temperature inner solar system material formed, was subsequently transferred to the Kuiper Belt, and was incorporated into comets several million years after CAI formation.
我们测量了一颗约 5 微米大小的 refractory 颗粒 Coki 的 26Al-26Mg 同位素体系,以将彗星内包体的形成时间尺度与陨石对应物联系起来。数据显示没有放射性 26Mg 的证据,并定义了颗粒形成时 26Al 丰度的上限:26Al/27Al < 1 x 10(-5)。26Al 的缺失表明 Coki 形成于太阳系中最古老的固体——富钙富铝包裹体 (CAI) 之后的 170 多万年。数据表明,高温的内太阳系物质形成后,随后被转移到柯伊伯带,并在 CAI 形成后数百万年被纳入彗星。