Jean-Guillaume Feignon
University of Vienna, Vienna
Activity
2021
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DO THE IMPACT MELT ROCKS WITHIN THE CHICXULUB IMPACT STRUCTURE PEAK RING (YUCATÁN PENINSULA, MEXICO) PRESERVE AN IMPACTOR SIGNATURE?
T241 The Cretaceous–Paleogene Boundary: From Impact Cratering Processes to Mass Extinction MechanismsWednesday, 13 October 20211:30 PM - 5:30 PMD139/D140
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SUEVITE EMPLACEMENT WITHIN THE CHICXULUB IMPACT STRUCTURE: NEW INSIGHTS FROM THE 2016 IODP-ICDP EXPEDITION 364 DRILLING
T241 The Cretaceous–Paleogene Boundary: From Impact Cratering Processes to Mass Extinction MechanismsWednesday, 13 October 20211:30 PM - 5:30 PMD139/D140
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NEW INSIGHTS INTO THE FORMATION AND EMPLACEMENT OF IMPACT MELT ROCKS WITHIN THE CHICXULUB IMPACT STRUCTURE, FOLLOWING THE 2016 IODP-ICDP EXPEDITION 364
T241 The Cretaceous–Paleogene Boundary: From Impact Cratering Processes to Mass Extinction MechanismsWednesday, 13 October 20211:30 PM - 5:30 PMD139/D140
2018
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INSIGHTS INTO IMPACT PROCESSES AND EXTINCTION MECHANISMS FROM IODP-ICDP CHICXULUB CRATER DRILLING
T139 Impact Cratering: Geologic, Geochemical, and Geophysical Signatures on the Terrestrial PlanetsMonday, 5 November 20181:30 PM - 5:30 PMRoom 235