Hello Listers

Its seems the meteorite world will also have a love for the Tunguska event 
curiosity will always keep us asking,
who, what , when, where, and why ..... Well something like. Well he is 
something like that, that might 
tell us more about the who, what and how. Take a look at the abstract below and 
enjoy.
  
 Shawn Alan
IMCA 1633
ebay store
http://stores.ebay.com/imca1633ny?_rdc=1http://meteoritefalls.com/
 
 
New evidence of meteoritic origin of the Tunguska cosmic body
 
Abstract
Diamond–lonsdaleite–graphite micro-samples collected from peat after the 1908 
catastrophic blast in the Tunguska area were studied with scanning (SEM) and 
transmission electron (TEM) microscopy, NanoSecondary Ion Mass Spectrometry 
(NanoSIMS) and Х-ray synchrotron technique. The high-pressure carbon allotropes 
in the Tunguska samples are being described for the first time and contain 
inclusions of FeS (troilite), Fe–Ni (taenite), γ-Fe and (FeNi)3P 
(schreibersite). The samples are nodule-like in shape and consist of 99.5% 
carbon minerals, e.g. diamond>lonsdaleite>graphite. Micro- and nanoinclusions 
of troilite (up to 0.5 vol%), taenite, γ-iron and schreibersite fill cracks, 
cleavages and pores in the carbon matrix. Carbon isotope studies from the two 
analyses of the Tunguska foil showed δ13C=‑16.0±1.9‰ and δ13C=‑15.2±2.1‰, 
suggesting δ13C=‑15.6±2‰ as an average characteristic of the carbon reservoir. 
That value is close to δ13C
 of some extraterrestrial samples. A negligible concentration of Ir and Os in 
the carbonaceous matrix promotes some controversial interpretation of the 
origin of the studied materials. Attributing this fact to the primary 
inhomogeneity, and considering the micro-structural features such as cracks, 
deformation of the crystal lattices, etc. coupled with high-pressure carbon 
allotropes association with metals, sulfides and phosphides, and the high ratio 
of Fe:Ni=22:1 suggest that the studied samples are meteorite micro-remnants. 
 
Planetary and Space Science, Volume 84, p. 131-140. (P&SS Homepage)
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