Reference Type | Journal (article/letter/editorial) |
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Access Rights | Open Access |
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Title | Allabogdanite, the high-pressure polymorph of (Fe,Ni)2P, a stishovite-grade indicator of impact processes in the Fe–Ni–P system |
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Journal | Scientific Reports |
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Authors | Britvin, Sergey N. | Author |
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Shilovskikh, Vladimir V. | Author |
Pagano, Renato | Author |
Vlasenko, Natalia S. | Author |
Zaitsev, Anatoly N. | Author |
Krzhizhanovskaya, Maria G. | Author |
Lozhkin, Maksim S. | Author |
Zolotarev, Andrey A. | Author |
Gurzhiy, Vladislav V. | Author |
Year | 2019 (December) | Volume | 9 |
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Publisher | Springer Science and Business Media LLC |
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Download URL | https://www.nature.com/articles/s41598-018-37795-x.pdf+ |
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DOI | doi:10.1038/s41598-018-37795-xSearch in ResearchGate |
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Classification | Not set | LoC | Not set |
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Mindat Ref. ID | 4789798 | Long-form Identifier | mindat:1:5:4789798:2 |
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GUID | 68c7627a-9789-4f69-8fe0-149a767f6176 |
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Full Reference | Britvin, Sergey N., Shilovskikh, Vladimir V., Pagano, Renato, Vlasenko, Natalia S., Zaitsev, Anatoly N., Krzhizhanovskaya, Maria G., Lozhkin, Maksim S., Zolotarev, Andrey A., Gurzhiy, Vladislav V. (2019) Allabogdanite, the high-pressure polymorph of (Fe,Ni)2P, a stishovite-grade indicator of impact processes in the Fe–Ni–P system. Scientific Reports, 9. doi:10.1038/s41598-018-37795-x |
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Plain Text | Britvin, Sergey N., Shilovskikh, Vladimir V., Pagano, Renato, Vlasenko, Natalia S., Zaitsev, Anatoly N., Krzhizhanovskaya, Maria G., Lozhkin, Maksim S., Zolotarev, Andrey A., Gurzhiy, Vladislav V. (2019) Allabogdanite, the high-pressure polymorph of (Fe,Ni)2P, a stishovite-grade indicator of impact processes in the Fe–Ni–P system. Scientific Reports, 9. doi:10.1038/s41598-018-37795-x |
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In | (2019) Scientific Reports Vol. 9. Springer Science and Business Media LLC |
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Abstract/Notes | Allabogdanite, (Fe,Ni)2P, is the only known natural high-pressure phase reported in the Fe–Ni–P system. The mineral, which was previously described from a single meteorite, the Onello iron, is now discovered in the Santa Catharina and Barbianello nickel-rich ataxites. The occurrence of allabogdanite in Santa Catharina, one of the largest and well-studied meteorites, suggests that this mineral is more common than was believed. The formation of allabogdanite-bearing phosphide assemblages in a given meteorite provides evidence that it experienced peak pressure of at least 8 GPa at a temperature above 800 °C. Since the pressure-temperature stability parameters of allabogdanite fall within the margins of the stishovite (rutile-type SiO2) stability area, the former can be employed as a convenient stishovite-grade indicator of significant impact events experienced by iron and stony-iron meteorites and their parent bodies. |
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