1967
DOI: 10.1126/science.155.3765.995
|View full text |Cite
|
Sign up to set email alerts
|

Hexagonal Diamonds in Meteorites: Implications

Abstract: A new polymorph of carbon, hexagonal diamond, has been discovered in the Canyon Diablo and Goalpara meteorites. This phase had been synthesized recently under specific high-pressure conditions in the laboratory. Our results: provide strong evidence that diamonds found in these meteorites were produced by intense shock pressures acting on crystalline graphite inclusions present within the meteorite before impact, rather than by disintegration of larger, statically grown diamonds, as some theories propose.

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

8
112
0
8

Year Published

1990
1990
2014
2014

Publication Types

Select...
5
3

Relationship

0
8

Authors

Journals

citations
Cited by 211 publications
(128 citation statements)
references
References 11 publications
8
112
0
8
Order By: Relevance
“…and Marvin [24] and by Hanneman et al [28]. The latter also observed dh diamond in Goalpara meteorites.…”
Section: Hexagonal Diamondmentioning
confidence: 64%
See 1 more Smart Citation
“…and Marvin [24] and by Hanneman et al [28]. The latter also observed dh diamond in Goalpara meteorites.…”
Section: Hexagonal Diamondmentioning
confidence: 64%
“…According to Hanneman et al [28]. their evidence indicates that cubic diamond cannot be transformed, even partially.…”
Section: Hexagonal Diamondmentioning
confidence: 99%
“…Diamond is reported to have a number of polytypes, of which lonsdaleite (also called hexagonal diamond) has received particularly intense attention. Lonsdaleite was first described almost 50 years ago from the Canyon Diablo iron meteorite 1,2 . 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] .…”
mentioning
confidence: 99%
“…Lonsdaleite was first described almost 50 years ago from the Canyon Diablo iron meteorite 1,2 . 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: 99%
“…A good understanding of this particular transition is important for gaining insight into shockinduced phase transformations, 2 study of meteorite impacts, 3,4 technological applications involving the synthesis of industrial diamonds, 5,6 and for linking the shock work to static high pressure -high temperature (HP-HT) studies. 7 Although gem quality diamonds can now be fabricated routinely using chemical vapor deposition (CVD) approaches, 23,24 a detailed understanding of the shock-induced graphite to diamond transformation remains an important scientific challenge.…”
Section: Introductionmentioning
confidence: 99%