Geological interpretation of gravity profiles through the Karlovy Vary granite massif (Czech Republic)

Abstract

Interpretation of gravity profiles across the Late Variscan Karlovy Vary massif confirms the concept of a tabular multiple intrusion about 10 km thick emplaced along the lower boundary of the Saxothuringian nappes.

Keywords

• Variscan granites
• gravity modeling
• Karlovy Vary Massif
• Western Bohemia
• Saxothuringian zone
• Eger graben