gtcrustГеодинамика и тектонофизикаGeodynamics & Tectonophysics2078-502XInstitute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch10.5800/GT-2010-1-1-0008gtcrust-99Research ArticleСОВРЕМЕННАЯ ГЕОДИНАМИКАRECENT GEODYNAMICSГЛУБИННАЯ ГЕОДИНАМИКА: ГРАНИЦЫ ПРОЦЕССА ПО ГЕОХИМИЧЕСКИМ И ПЕТРОЛОГИЧЕСКИМ ДАННЫМDEEP-LEVEL GEODYNAMICS: BOUNDARIES OF THE PROCESS ACCORDING TO GEOCHEMIC AND PETROLOGIC DATAИвановАлексей ВикторовичIvanovAlexei V.

канд. геол.-мин. наук, с.н.с.,

664033, Иркутск, ул. Лермонтова, 128

Candidate of Geology and Mineralogy, Senior Researcher,

128 Lermontov street, Irkutsk 664033

aivanov@crust.irk.ruИнститут земной коры СО РАНРоссияInstitute of the Earth’s Crust, Siberian Branch of RASRussian Federation2010120920151187102Copyright © Иванов А.В., 20152015Иванов А.В.Ivanov A.V.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.gt-crust.ru/jour/article/view/99

Проведен анализ геохимических характеристик вулканических пород и петрологических данных по глубинным включениям, которые могут быть использованы для оценки обмена веществом между различными геосферами Земли. Несмотря на то, что обычно рассматривается возможность субдуцирования слэбов вплоть до границы ядро–мантия и последующего возвращения материала в область подлитосферной магмогенерации в форме мантийных плюмов, петрологические доказательства самого глубокого поступления вещества на поверхность ограничиваются верхними горизонтами нижней мантии (~650–700 км), т.е. глубиной самых глубоких землетрясений. Включения ферропериклаза в некоторых алмазах не опровергают вовлечение и более глубоких горизонтов мантии, однако не дают этому однозначного подтверждения. Геохимические данные также не дают однозначного подтверждения вовлечения вещества нижней мантии в процессы магмогенерации под вулканически активными районами. В то же время они свидетельствуют о полной вещественной изоляции ядра от верхнемантийных процессов.

Geochemical features for volcanic rocks and petrologic data for deep-seated inclusions, which can be used to infer mass transfer between different geospheres, are reviewed. It is typically believed that slabs can subduct as deep as the core-mantle boundary with the following recycling by plumes coming up to the sublithospheric regions of magma generation. However, the petrologic evidence of the deepest accessible material is limited by the depth of the uppermost lower mantle (~650–700km), i.e. by the depth of the deepest earthquakes. Ferropericlase inclusions in some diamonds do not exclude involvement of deeper mantle horizons, yet do not unambiguously support it. No unambiguous confirmation of involvement of the lower mantle into magma generation underneath volcanically active regions is obtained from geochemical data either, while the geochemical data suggest complete chemical isolation of the Earth’s core from the upper mantle processes.

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The authors declare that there are no conflicts of interest present.