Michal Filippi
Insitute of Geology, Academy of Sciences of the Czech Republic, Praha 9, N/A
Activity
2010
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CAN INCREASE IN ARIDITY TRIGGER RAPID SURFACE EROSION OF DIAPIRS AND INTENSIFY THE BRINE FLOW? (EVAPORATE KARST IN ZAGROS MOUNTAINS, IRAN)
223 Environmental GeosciencesWednesday, 3 November 20108:00 AM - 12:00 PMMile High Ballroom Prefunction
2009
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EVOLUTION OF SALT DIAPIR TOPOGRAPHY AND KARST MORPHOLOGY DURING LAST GLACIAL CYCLE (PERSIAN GULF, IRAN)
T150 Toward Integrating Cave and Karst ScienceTuesday, 20 October 20098:00 AM - 12:00 PMD139/140