Abstract
Metallic, micron sized Fe-Ni spherules are frequently reported from
glasses formed during impact processes. They have a high preservation
potential and are a valid indicator of impactor type.
However, the details of their formation remain obscure and their
potential as specific indicator of impact details unexploited.
In this work on the impact glass from Wabar we report on of the
relation between the simple spherules themselves and the hosting glass
using SEM, and a detailed study of the spherules using a combination of
FIB/SEM reconstruction and TEM.
Overall, we identified a late stage differential contraction of the
spherules in the hosting glass, facilitating mechanical separation of the
spherules from the host. The structure of the spherules is consistent with
entry of a small nugget of the meteorite and some associated air into the
molten glass. The spherical shape is acquired as the molten glass induces
melting of the metal and its minor components. While the metal is molten
a density related differentiation of the light components like iron sulfide
and voids results in the accumulation of these at or close to the surface of
the spheres.
With these principal processes being established the huge variation
in the detailed sphere morphology can be rationalized.
Original language | English |
---|---|
Article number | 5490 |
Journal | Meteoritics and Planetary Science |
Volume | 46 |
Issue number | Supplement s1 |
Pages (from-to) | A206-A206 |
ISSN | 1086-9379 |
DOIs | |
Publication status | Published - 2011 |
Externally published | Yes |
Event | 74th Annual Meeting of the Meteoritical-Society - University of Greenwich, London, United Kingdom Duration: 8 Aug 2011 → 12 Aug 2011 Conference number: 74 |
Conference
Conference | 74th Annual Meeting of the Meteoritical-Society |
---|---|
Number | 74 |
Location | University of Greenwich |
Country/Territory | United Kingdom |
City | London |
Period | 08/08/2011 → 12/08/2011 |