Maximum temperatures during the formation of the solar nebula

Most numerical models of cloud collapse yield the result that temperatures were never above 1000 K at distances not less than 1 AU from the axis of the forming solar system. In contrast, most meteorite researchers hold that higher temperatures are necessary to account for a variety of elemental fractionations found between groups of meteorites, between members of a single group, and between components of a single meteorite. A summary of the researchers' viewpoint is presented. An investigation is conducted of the evidence which indicates that chondrites were formed in the solar nebula. Attention is also given to the maximum nebular temperatures during the formation of chondrites.