On the stability of tectonic boundary between Eurasia and pacific peat
Автор: Zhirnov A.M.
Журнал: Региональные проблемы @regionalnye-problemy
Рубрика: Геология. Природные ресурсы
Статья в выпуске: 1 т.14, 2011 года.
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A constant position of the border between the continental sialic crust and the Pacific Ocean ultramafite crust is substantiated by the author. The main proof is a steady position of these types of crust on different sides of the deepwater rift during all geological time. (3.5-4.5 milliard years)
The end of the continent, the archaean and pre-archaean (katarchaean), sialic crystal crust, the pacific ocean ultramafite crust, the deepwater rift's axis line, border, constant position of the border
Короткий адрес: https://sciup.org/14328743
IDR: 14328743
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