2018
DOI: 10.1038/s41598-018-25037-z
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Spectroscopic features of ultrahigh-pressure impact glasses of the Kara astrobleme

Abstract: The state of substances under ultrahigh pressures and temperatures (UHPHT) now raises a special interest as a matter existing under extreme conditions and as potential new material. Under laboratory conditions only small amounts of micrometer-sized matter are produced at a pressure up to 100 GPa and at room temperature. Simultaneous combination of ultrahigh pressures and temperatures in a lab still requires serious technological effort. Here we describe the composition and structure of the UHPHT vein-like impa… Show more

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Cited by 23 publications
(27 citation statements)
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“…As mentioned above, a typical impact UHP stage lasts just a fraction of a second. The common melt rocks in the Kara astrobleme, including massive melt bodies and clastic glasses 25 , do not feature evidence of long-duration UHP conditions, do not contain melt-crystallized coesite and have different chemical compositions. Therefore, the initial impact melt did not experience long-duration UHP conditions and cannot have been the source of the studied UHPHT glass veins.…”
Section: Smectite (Crystallized Hydrous Aluminosilicate Melt)mentioning
confidence: 99%
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“…As mentioned above, a typical impact UHP stage lasts just a fraction of a second. The common melt rocks in the Kara astrobleme, including massive melt bodies and clastic glasses 25 , do not feature evidence of long-duration UHP conditions, do not contain melt-crystallized coesite and have different chemical compositions. Therefore, the initial impact melt did not experience long-duration UHP conditions and cannot have been the source of the studied UHPHT glass veins.…”
Section: Smectite (Crystallized Hydrous Aluminosilicate Melt)mentioning
confidence: 99%
“…Among the numerous known impact structures, the Kara astrobleme (Russia) is one of the largest astroblemes in which ultrahigh-pressure and high-temperature (UHPHT) glasses have been found 25 . Based on the SiO 2 phase state diagram 15,19 , previous experiments, the definition of an emerging shock temperature during the impact, and theoretical calculations 26 , the observed coesite in the SiO 2 glasses of the Kara astrobleme 20,25,27 correspond to an impact-induced melt temperature greater than 1700 °C. Thus, the impact melt products of the Kara astrobleme are very attractive from not only a fundamental point of view but also considering the probable practical use of impact glass 25 .…”
mentioning
confidence: 99%
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“…4). According to the data from silicate rock analysis and energy dispersive spectral analysis, the suevites and melt rocks of the Kara astrobleme are mainly represented by an aluminosilicate component with admixtures of silicate, carbonate, and sulfide components (Shumilova et al, 2018b). To supplement the specifics of previously identified varieties of suevites, we determined the nature of the distribution of each of these components, which primarily depended on the phase contrast on the tomograms.…”
Section: Mineral Reference Specimensmentioning
confidence: 99%