The dynamic model of the formation of igneous rocks of the Harz mountains

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The present paper describes a petrological-geochemical model of migration in the Harz mountains. The tolaidic magmatic core changed direction from southeast to northwest which led to stepwise alteration of the melting. Reasons for chemical alteration are progressing palingenesis, magmatic displacement and metasomatosis.

Model, harz mountains, granitoids, palingenesis, metasomatosis, tectonic stresses, variscan slip zone

Короткий адрес: https://sciup.org/146114839

IDR: 146114839

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