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Department of Geological Sciences, University of Vienna, Althanstrasse 14, A-1090 Vienna, Austria
Delayed climate cooling in the Late Eocene caused by multiple impacts: high-resolution geochemical studies at Massignano, Italy
Do SNC Noble Gas and Deuterium Data Provide Evidence for Large Cometary Impact Between 1300 300 Ma on Mars?
Estimation of the past and present Martian water-ice reservoirs by isotopic constraints on exchange between the atmosphere and the surface
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