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Source: Large igneous provinces and their plumbing system. 2022. P. 1-16
Type: статьи в сборниках
Date: 2022
Description:
Identification of large-volume, short-duration mafic magmatic events of intraplate affinity in both continental and oceanic settings on the Earth and other planets provides invaluable clues for unders
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Source: Geology. 2020. Vol. 48, № 2. P. 159-163
Type: статьи в журналах
Date: 2020
Description:
The most dominant features in the present-day lower mantle are the two antipodal African and Pacific large low-shear-velocity provinces (LLSVPs). How and when these two structures formed, and whether
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Source: Precambrian research. 2019. Vol. 323. P. 1-5
Type: статьи в журналах
Date: 2019
Description:
The supercontinent cycle of episodic assembly and breakup of almost all continents on Earth is commonly considered the longest period variation to affect mantle convection. However, global zircon Hf i
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Source: Петрология магматических и метаморфических комплексов : материалы IX Всероссийской конференции с международным участием, 28 ноября - 2 декабря 2017 года. Томск, 2017. Вып. 9. С. 15
Type: статьи в сборниках
Date: 2017
Source: Петрология магматических и метаморфических комплексов : материалы IX Всероссийской конференции с международным участием, 28 ноября - 2 декабря 2017 года. Томск, 2017. Вып. 9. С. 9
Type: статьи в сборниках
Date: 2017
Authors:
Ernst, Richard E. |
Söderlund, Ulf |
Hanes, J. A. |
Gladkochub, D. P. |
Okrugin, A. V. |
Kolotilina, T. B. |
Mekhonoshin, A. S. |
Bleeker, Wouter |
LeCheminant, A. N. |
Hamilton, Mike А. |
Buchan, Kenneth L. |
Chamberlain, Kevin R. |
Didenko, A. N.
Source: Nature geoscience. 2016. Vol. 9, № 6. P. 464-469
Type: статьи в журналах
Date: 2016
Description:
Precambrian supercontinents Nuna-Columbia (1.7 to 1.3 billion years ago) and Rodinia (1.1 to 0.7 billion years ago) have been proposed. However, the arrangements of crustal blocks within these superco
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Source: Precambrian research. 2015. Vol. 259. P. 222-231
Type: статьи в журналах
Date: 2015
Description:
We present results from a paleomagnetic study of the previously undated Erayinia dykes intruding thesouth-western Yilgarn Craton. The U–Pb TIMs baddeleyite age of these dykes is now 2401 ± 1 Ma, which
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