GEOLOGICAL CONDITIONS OF HARZ MAGMATIC COMPLEX

(Federal Republic of Germany)

Authors

  • I. K. Klish Chair of Mineralogy, Petrology and Geochemistry, YSU, Armenia

DOI:

https://doi.org/10.46991/PYSU:C/2008.42.1.125

Keywords:

Harz, Germany, banatite-granitoide formation, harzburgite-gabbro formation, Harburg, Broken, Ramberg, Oker and Bode dyke

Abstract

The Harz massif is located in the northern part of the area of Germany. The Harz rocks compose geologically hard, horst, strongly metamorphized upper-paleozoic complex with mainly developed Devon and lower-carbon formations. Plutonic formations like harzburgite-gabbro and banatite-granitoide formation to which are related the massifs Harburg, Broken, Ramberg, Oker and Bode dyke are typical for Harz.

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Published

2008-01-10

How to Cite

Klish, I. K. (2008). GEOLOGICAL CONDITIONS OF HARZ MAGMATIC COMPLEX: (Federal Republic of Germany). Proceedings of the YSU C: Geological and Geographical Sciences, 42(1 (215), 125–133. https://doi.org/10.46991/PYSU:C/2008.42.1.125

Issue

Vol. 42 No. 1 (215) (2008)

Section

Geology

License

Copyright (c) 2008 Proceedings of the YSU

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