Enigmatic gravity-flow deposits at Ujście (western Poland), triggered by earthquakes (as evidenced by seismites) caused by Saalian glacioisostatic crustal rebound
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DOI: 10.1016/j.geomorph.2018.01.010
Abstract: Abstract Two breccia layers occur directly stacked upon each other in a silty/sandy Saalian glaciolacustrine succession near Ujście (western Poland). This complex is exceptional because of two aspects: the two breccia layers consist of distinctly… read more here.
Keywords: gravity flow; gravity; breccia; cie western ... See more keywords