On the challenging gabbro in the intrusions of the peridotite-pyroxenite-gabbronorite formation by the example of the geological structure of the Fedorova tundra top intrusion
Автор: Groshev N.Yu.
Журнал: Вестник Мурманского государственного технического университета @vestnik-mstu
Рубрика: Геология
Статья в выпуске: 3 т.12, 2009 года.
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The typical area with widespread rocks of the "gabbro" mineral association (Pl+Amp) within the Fedorova Tundra intrusive has been studied. It has been shown that "gabbro" is a result of autometamorphic reworking of rocks with the three-mineral gabbronoritic association - Pl+Opx+Cpx.
Layered intrusions, gabbro, fluidization
Короткий адрес: https://sciup.org/14294078
IDR: 14294078
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