Abstract
A comparative study of sulfide minerals in ordinary chondrites Chelyabinsk, Northwest Africa 869 and Gao-Guenie was carried out using X-ray diffraction, optical microscopy and scanning electron microscopy. Unit cell parameters were obtained for minerals: troilite, pyrrhotite, and pentlandite. A small amount of copper was revealed in LL chondrite Chelyabinsk, while its content in the metal and sulfide grains of H and L chondrites was below detection limit. Unit cell parameters for sulfides from the Chelyabinsk and Northwest Africa 869 chondrites were obtained.
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Acknowledgments
The authors are grateful to V.I. Nekrasov and to V.I. Grokhovsky for the samples. This work was supported in part by the Development Program of the Crimean Federal University under the project “Academic Mobility of Young Scientists of Russia—AMMUR” in the Ural Federal University, by the Ministry of Education and Science (Project # 5.3451.2017/4.6), by the Act 211 of the Government of the Russian Federation, agreement no. 02.A03.21.0006.
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Hontsova, S.S., Maksimova, E.M., Petrova, E.V., Danilenko, I.A., Nauhatsky, I.A., Yakovlev, G.A. (2020). Sulfide Minerals in Ordinary Chondrites Chelyabinsk, Northwest Africa 869 and Gao-Guenie. In: Votyakov, S., Kiseleva, D., Grokhovsky, V., Shchapova, Y. (eds) Minerals: Structure, Properties, Methods of Investigation. Springer Proceedings in Earth and Environmental Sciences. Springer, Cham. https://doi.org/10.1007/978-3-030-00925-0_8
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