Variations in magnetic anisotropy and opaque mineralogy along a kilometer deep profile within a vertical dyke of the syenogranite porphyry at Cinovec (Czech Republic)

Abstract

Vertical variations in magnetic fabric and paragenesis of the ferrimagnetic minerals for a virtually upright dyke of the Altenberg syenogranite porphyry were investigated using profile data of borehole E-16 to a depth of 922.7 in (Eastern Krunsn

Keywords

• magnetic anisotropy
• granite porphyry
• Bohemian Massif