Following the distribution at The 53rd Annual Meeting of the
Meteoritical Society of 40 kg of Cretaceous-Tertiary boundary layer
clay (Fish Clay) recovered from Stevns Klint, Denmark, a magnetic
analysis of both the coarse and fine fractions was carried out. The
magnetic mineralogy was found to be complex, consisting of
single-domain magnetite and fine-grained sulphides of Fe. The Fe
sulphide was
... [Show full abstract] present as ferrimagnetic pyrrhotite
(Fe7S8) and other sulphides that decayed on
heating to produce magnetite. A magnetic fraction of the material was
separated by using a strong hand magnet. The separate from the coarse
fraction was found to contain low-Ni,Fe (TC = 750-770
°C) in trace quantities. Since contamination seems unlikely, it
must be concluded that the Fe has an extraterrestrial origin. Whilst
partially-degraded cosmic spherules may add to the signal, their input
is believed to be insignificant. The other obvious source is debris
from the vapourization of a K/F impactor.