minerals Article Studying the Stability of the K/Ar Isotopic System of Phlogopites in Conditions of High T, P: 40Ar/39Ar Dating, Laboratory Experiment, Numerical Simulation Denis Yudin 1 , Nikolay Murzintsev 1, Alexey Travin 1,2,*, Taisiya Alifirova 1,3 , Egor Zhimulev 1 and Sofya Novikova 1 1 V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academyof Sciences, 3 Academician Koptyug ave., 630090 Novosibirsk, Russia;
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[email protected] (S.N.) 2 Faculty of Geology and Geography, National Research Tomsk State University, 634050 Tomsk, Russia 3 Department of Lithospheric Research, University of Vienna, Althanstraße 14/UZA2, 1090 Vienna, Austria * Correspondence:
[email protected] Abstract: Typically, 40Ar/39Ar dating of phlogopites from deep-seated xenoliths of kimberlite pipes produces estimates that suggest much older ages than those when these pipes were intruded. High- pressure (3 GPa) laboratory experiments enabled the authors to explore the behaviour of argon in the phlogopite structure under the conditions that correspond to the mantle, at the temperatures (from 700 to 1000 ◦C), far exceeding closure temperature of the K/Ar isotopic system. “Volume diffusion” Citation: Yudin, D.; Murzintsev, N.; remains foremost for describing the mobility of argon in phlogopite at high pressures. The mantle Travin, A.; Alifirova, T.; Zhimulev, E.; material age can be estimated through the dating of the phlogopites from deep-seated xenoliths of Novikova, S. Studying the Stability of kimberlites, employing the 40Ar/39Ar method, subject to correction for a partial loss of radiogenic the K/Ar Isotopic System of 40Ar when xenolith moves upwards to the Earth’s surface.