Lead Isotope composition and origin of the quaternary lavas of Elbrus Volcano, the Greater Caucasus: High-precision MC-ICP-MS data

Author:

Chugaev A. V.,Chernyshev I. V.,Lebedev V. A.,Eremina A. V.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology

Reference36 articles.

1. Abikh, G.V., Explanation of Geological Section of the Northern Slope of the Caucasus Range from Elbrus to Beshtau, Kavkazskii Kalendar na 1853 g. (Caucasian Calendar for 1853), Tiflis: 1852, pp. 440–471.

2. Allegre, C.J. and Lewin, E., Chemical Structure and History of Earth: Evidence from Global Non-Liner Inversion of Isotopic Data in a Three-Box Model, Earth Planet. Sci. Lett., 1989, vol. 96, pp. 61–88.

3. Andrieu, A.S., Honnorez, J.J., and Lancelot, J., Lead Isotope Compositions of the TAG Mineralization, Mid-Atlantic Ridge, 26°08′ N, Proc. Ocean Drill. Program, Sci. Results, 1998, vol. 158, pp. 101–109.

4. Bogatikov, O.A., Melekestsev, I.V., Gurbanov, A.G., et al., Radiocarbon Dating of Holocene Eruptions of the Elbrus Volcano in the Northern Caucasus, Russia, Dokl. Earth Sci., 1998, vol. 363, pp. 1093–1095.

5. Bogatikov, O.A., Zalikhanov, M.Ch., Karamurzov, B.S., et al., Prirodnye protsessy na territorii Kabardino-Balkarii (Natural Processes on the Territory of Kabardino-Balkaria), Moscow: IGEM RAN, 2004.

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