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      The hypabyssal magmatites resulted by magma penetration into fissure or fracture zones (dikes) or into discontinuities along bedding planes (sills). They are often bound to the plutonite bodies and their surroundings. They sometimes occur in groups, so called dike swarms, which might be as much as several dozens of kilometres long (their composition correponds mostly to basic basaltoids).

porfyr křemenný v nadloží west g1763	porfyr, puklinatý, g5067	písmenkový pegmatit g6506	sodný pegmatit g6511	pegmatit g7430
žíla - pegmatitová g7433	pegmatit - mylonitizovaný g7436

In the Virtual Museum there are total 159 samples