IMPRINTS OF PLUME PROCESSES IN THE MODERN LITHOSPHERIC VELOCITY STRUCTURE OF THE KHIBINO-LOVOZERO REGION

V. V. Adushkin; Адушкин В. В.; A. G. Goev; Гоев А. Г.

doi:10.31857/S2686739723601527

IMPRINTS OF PLUME PROCESSES IN THE MODERN LITHOSPHERIC VELOCITY STRUCTURE OF THE KHIBINO-LOVOZERO REGION

Autores: Adushkin V.¹, Goev A.¹
Afiliações:
1. Sadovskiy Institute of Geosphere Dynamics Russian Academy of Sciences
Edição: Volume 513, Nº 1 (2023)
Páginas: 106-111
Seção: ГЕОДИНАМИКА
URL: https://journals.rcsi.science/2686-7397/article/view/232986
DOI: https://doi.org/10.31857/S2686739723601527
EDN: https://elibrary.ru/LMCMEG
ID: 232986

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Resumo

The paper presents new deep velocity of the earth’s crust and upper mantle in the Khibiny-Lovozero tectonic region located on the Kola Peninsula. The artifacts of plume-lithospheric interactions that occurred in the investigated area from the Proterozoic to the Paleozoic time are discussed. A detailed comparison of the velocity structure of the Imandra-Varzug rift, the Khibiny and Lovozero plutons, and the adjacent Archean part of the Fennoscandinavian Shield has been carried out. A significant heterogeneity of the structure of the crust, upper mantle, as well as the structure and depth of the crust-mantle transition is shown. The presence of a zone of low seismic velocities in the upper mantle associated with the mid-lithospheric discontinuity (MLD) has been revealed. Structural features of the Moho zone and the upper mantle in the region of the Khibiny and Lovozero plutons were interpreted as artifacts of the plume process.

Palavras-chave

Kola region, receiver functions, shear waves, upper mantle, plume, mid-lithospheric discontinuity

Sobre autores

V. Adushkin

Sadovskiy Institute of Geosphere Dynamics Russian Academy of Sciences

Email: andr.goev@gmail.com
Russian Federation, Moscow

A. Goev

Sadovskiy Institute of Geosphere Dynamics Russian Academy of Sciences

Autor responsável pela correspondência
Email: andr.goev@gmail.com
Russian Federation, Moscow

Bibliografia

Chashchin V.V., Mitrofanov F.P. The Paleoproterozoic ImandraVarzugavrifting structure (Kola Peninsula): intrusive magmatism and minerageny // Geodynamics & Tectonophysics. 2014. V. 5. № 1. P. 231–256.
Шарков Е.В., Богатиков О.А., Красивская И.С. Роль мантийных плюмов в тектонике раннего докембрия восточной части Балтийского щита // Геотектоника. 2000. Т. 2. С. 3–25.
Pesonen L.J., Elming S.A., Mertanen S., Pisarevsky S., D’Agrella-Filho M.S., Meert J.G., Schmidt P.W., Abrahamsen N., Bylund G. Palaeomagnetic configuration of continents during the Proterozoic // Tectonophysics. 2003. V. 375. P. 289–324.
Mitrofanov F.P., Bayanova T.B. Duration and timing of orebearing Paleoproterozoic intrusions of Kola province // In: Mineral deposits: Processes to Processing. 1999. Balkena, Rotterdam, P. 87–93.
Mitrofanov F.P., Bayanova T.B., Korchagin A.U., Groshev N.Yu., Malitch K.N., Zhirov D.V., Mitrofanov A.F. East Scandinavian and Noril’sk plume mafic large igneous provinces of Pd–Pt ores: geological and metallogenic comparison // Geology of Ore Deposits. 2013. V. 55. № 5. P. 305–319.
Егоркин А.В., Галдин Н.Е., Зюганов С.К., Кагалова Л.И. Выделение блоков древнейшей коры Балтийского щита по профилю МОВЗ-ГСЗ Печенга-Умбозеро-Ручьи / Проблемы комплексной интерпретации геолого-геофизических данных. Отв. ред. В.А. Глебовицкий, Н.В. Шаров. Л., Наука. 1991. С. 107–122.
Павленкова Н.И., Павленкова Г.А. Строение земной коры и верхней мантии Северной Евразии по данным сейсмического профилирования с ядерными взрывами. М., ГЕОКАРТ: ГЕОС. 2014. Вып. 5. 192 с.
Dricker I.G., Roecker S.W., Kosarev G.L., Vinnik L.P. Shear-wave velocity structure of the crust and upper mantle beneath the Kola peninsula// Geophys. Res. Let. 1996. V. 23. № 23. P. 3389–3392.
Гоев А.Г., Санина И.А., Орешин С.И., Резниченко Р.А., Тарасов С.А., Федоров А.В. Скоростное строение литосферы Хибинского и Ловозерского массивов (северо-восточная часть Балтийского щита) методом функции приемника // Физика Земли. 2021. № 5. С. 30–40.
Винник Л.П. Сейсмология приемных функций // Физика Земли. 2019. № 1. С. 16–27.
Vinnik L., Deng Y., Kosarev G., Oreshin S., Makeyeva L. Permian plume beneath Tarim from receiver functions // Journal of Geophysical Research: Solid Earth. 2018. V. 9. P. 1179–1185.
Алешин И.М. Построение решения обратной задачи по ансамблю моделей на примере инверсии приемных функций // ДАН. Науки о Земле. Т. 496. № 1. 2021. С. 63–66.
Fu H.Y., Li Z.H., Chen L. Continental mid-lithosphere discontinuity: A water collector during craton evolu-tion // Geophysical Research Letters. 2022. V. 49. e2022GL101569.
Thybo H. The heterogeneous upper mantle low velocity zone // Tectonophysics. 2006. V. 416. P. 53–79.
Karato S.I., Park J. On the origin of the upper mantle seismic discontinuities // Lithospheric Discontinuities. 2018. P. 5–34.
Eeken T., Goes S., Pedersen H.A., Arndt N.T., Bouilhol P. Seismic evidence for depth-dependent metasomatism in cratons // Earth and Planetary Science Letters. 2018. V. 491. P. 148–159.