That was part of the title of a session on the formation of
chondrules at the 75th annual Meteoritical Society meeting last year.134
Not exact matches
However, researchers
at MIT and Purdue University have now found that
chondrules may have played less of a fundamental role.
Previous experiments in the lab have shown that
chondrules cool down
at a rate of 10 to 1,000 kelvins per hour — a rate that would produce the texture of
chondrules seen in meteorites.
Johnson predicts that oblique impacts, or collisions occurring
at an angle, may be even more efficient
at producing molten plumes of
chondrules.
During the simulations, it was found that the planetary bodies would have to strike each other
at a rate of 2.5 km (1.6 miles) per second to produce an impact plume with molten droplets that would cool
at the correct rate to create
chondrules with the characteristics we observe today.
Although
chondrules evolved in outer space where temperatures are almost -460 °F (492 °F below freezing), they required sudden melting temperatures of
at least 3,000 °F.