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Thermobarometry of Inclusions: Implications to the Structure of Lithospheric Mantle and Evolution in Time and Diamond Formation

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摘要 Thermobarometric calculations for mineral diamond inclusions and associations(DIA)provide a systematic comparison of PTXFO2 conditions for different cratons worldwide,using a database of 4440 mineral EPMA analyses(Ashchepkov et al.,2021).
出处 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2021年第S01期18-21,共4页 地质学报(英文版)
基金 supported by the RFBR grant 19-05-00788 supported by the Ministry of Science and Higher Education of the Russian Federation
作者简介 the first and corresponding author:Igor V.ASHCHEPKOV,male,born in 1957 in Khabarovsk city,Russia.Graduated in 1975 from mathematical class Sch11 in Novokuznetsk city.In 1975,he entered and in 1980 graduated from Novosibirsk State University.In 1980–1989,he worked at the Geological Institute SB RAS in Ulan-Ude.In 1986,PHD“Deep xenoliths of alkaline basalts of the Vitim Plateau”.In 1989–2021,he worked at the N.V.Sobolev’s Institute of Geology and Mineralogy of the SB RAS.From 1994 to 2021,he led the 7th grats of the Russian Foundation for Basic Research.From 2002–2008,he led 3 contractual works with ALROSA.From 2012 to 2021,leed covener of sessions in General Assembly of European Geoscience Union.He was the responsible editor of special issues of Geoscience Frontiers(2017,N8)and in 2020-2021–Minerals.E-mail:ashchepkov.igor@igm.nsc.ru
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