A large meteoritic event over Antarctica ca. 430 ka ago inferred from chondritic spherules from the Sør Rondane Mountains
Large airbursts, the most frequent hazardous impact events, are estimated to occur orders of magnitude more frequently than crater-forming impacts. However, finding traces of these events is impeded by the difficulty of identifying them in the recent geological record. Here, we describe condensation...
Main Authors: | , , , , , , , , , |
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Format: | Text |
Language: | unknown |
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Freie Universität Berlin
2021
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Online Access: | https://dx.doi.org/10.17169/refubium-30392 https://refubium.fu-berlin.de/handle/fub188/30653 |