Moldanubian

The Moldanubian is a geological domain or orogenic belt in central Europe, characterized by its complex geological history. It is a region of high tectonic activity, where multiple tectonic plates collided during the Paleozoic and Mesozoic eras. The Moldanubian domain stretches across parts of the Czech Republic, Austria, and Germany, and forms part of the larger Variscan mountain belt.

The Moldanubian domain is primarily composed of metamorphic and igneous rocks, formed as a result of intense tectonic activity. These rocks date back to the Cadomian and Variscan orogenies, which occurred around 560-250 million years ago. The region has undergone several phases of mountain building, resulting in the formation of a complex crust that is rich in minerals such as gold, copper, and lead.

Geologically, the Moldanubian domain can be divided into several sub-domains, each with its own unique characteristics. The Mariánské Lázně sub-domain, located in the Czech Republic, is notable for its high levels of quartzite and other metamorphic rocks. The Poběžovice sub-domain, also in the Czech Republic, is characterized by a high concentration of granite and other igneous rocks.

The Moldanubian domain has been shaped by numerous geological events over millions of years, resulting in a region of high petrographic and structural complexity. Its unique geological features and history have made it a subject of interest for geologists and researchers, who continue to study the region to better understand its geological history and resources.