Lamproites of Kayla pipe and their mantle xenocrysts, SE Aldan shield, Russia: Geochemistry and petrology

Author:

Vladykin N V,Ashchepkov I VORCID,Sotnikova I A,Medvedev N S

Funder

Российский Фонд Фундаментальных Исследований

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference136 articles.

1. Adam J, Green T H and Sie S H 1993 Proton microprobe determined partitioning of Rb, Sr, Ba, Y, Zr, Nb and Ta between experimentally produced amphiboles and silicate melts with variable F content; Chem. Geol. 109 29–49, https://doi.org/10.1016/0009-2541(93)90060-V.

2. Artemieva I M and Mooney W D 2001 Thermal structure and evolution of Precambrian lithosphere: A global study; J. Geophys. Res. 106 16,387–16,414.

3. Atkinson W, Smith C and Boxer G 1984 The discovery and geology of the Argyle diamond deposits, Kimberley, Western Australia; In: Proceedings of the Darwin Conference, Australasian Institute of Mining and Metallurgy, Darwin City, Australia, pp. 141–149.

4. Ashchepkov I, Gerasimov P, Khmel’nikova O, Anoshin G, Vladykin N and Saprykin A 2001 A Temperature gradient and structure of the lithospheric block beneath the southeastern margin of the Siberian craton: Disintegrated xenolith evidence from kimberlitic pipes of the Aldan shield; Dokl. Earth Sci. 378 495–499.

5. Ashchepkov I V, André L, Downes H and Belyatsky B A 2011 Pyroxenites and megacrysts from Vitim picrite-basalts (Russia): Polybaric fractionation of rising melts in the mantle?; J. Asian Earth Sci. 42 14–37, https://doi.org/10.1016/j.jseaes.2011.03.004.

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