2013
DOI: 10.1016/j.pss.2013.05.003
|View full text |Cite
|
Sign up to set email alerts
|

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 Attributing this fact to the primary inhomogeneity, and considering the microstructural features such as cracks, deformation of the crystal l… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

1
23
0
1

Year Published

2014
2014
2024
2024

Publication Types

Select...
5
2

Relationship

0
7

Authors

Journals

citations
Cited by 30 publications
(25 citation statements)
references
References 40 publications
(35 reference statements)
1
23
0
1
Order By: Relevance
“…A cylinder of high purity graphite was used as a starting material. The cylinder was enclosed in a Ta capsule, pressurized to 19 GPa and heated at 2,473 K for 5 min, the conditions that correspond to those reported by 7 , where 'retrievable hexagonal-type diamond' occurs. The temperature was monitored with a W 3 Re/W 25 Re thermocouple located axially with respect to the heater, with a junction close to the Ta capsule.…”
Section: Methodsmentioning
confidence: 99%
See 3 more Smart Citations
“…A cylinder of high purity graphite was used as a starting material. The cylinder was enclosed in a Ta capsule, pressurized to 19 GPa and heated at 2,473 K for 5 min, the conditions that correspond to those reported by 7 , where 'retrievable hexagonal-type diamond' occurs. The temperature was monitored with a W 3 Re/W 25 Re thermocouple located axially with respect to the heater, with a junction close to the Ta capsule.…”
Section: Methodsmentioning
confidence: 99%
“…Its formation was attributed to shock-induced transformation of graphite within the meteorite upon impact with Earth, and its occurrence was used as an indicator of shock [1][2][3] . It has since been reported from several meteorites as well as from terrestrial sediments and has been attributed to asteroidal impacts, both extraterrestrial and on Earth [4][5][6][7] .…”
mentioning
confidence: 97%
See 2 more Smart Citations
“…Angular lonsdaleite crystals also formed in some impact events via shock metamorphism of graphite in the target rocks (Hough et al 1997;Koeberl et al 1997;Langenhorst et al 1998;DeCarli et al 2002;Oleinik et al 2003). Lonsdaleite grains have been reported in impact events, e.g., Ries Crater, the K-Pg event (Bunch et al 2008), and the 1908 Tunguska airburst in Siberia (Bunch et al 2008;Kvasnytsya et al 2013). Although lonsdaleite is known to be formed through shock metamorphism during surface impacts, its presence at the site of the Tunguska airburst indicates that it also can form during cosmic airbursts.…”
Section: Potential Origin From Volcanism or In The Mantlementioning
confidence: 99%