Detected movements evidenced WSW-ENE extension with subsiding trends in the western part of the Cheb basin and the Smrčiny Mts. There were monitored dextral movements along the Mariánské Lázně tectonic fault zone (MLF). An antithetic stress pattern has to exist inside the inner part of the MLF tectonic zone.
Detected movements evidenced WSW-ENE extension with subsiding trends in the western part of the Cheb basin and the Smrčiny Mts. There were monitored dextral movements along the Mariánské Lázně tectonic fault zone (MLF). An antithetic stress pattern has to exist inside the inner part of the MLF tectonic zone. (en)