40Ar‐39Ar ages of H‐chondrite impact melt breccias |
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| Authors: | Timothy D SWINDLE Clark E ISACHSEN John R WEIRICH David A KRING |
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| Institution: | 1. Lunar and Planetary Laboratory, The University of Arizona, Tucson, Arizona 85721‐0092, USA;2. Department of Geosciences, The University of Arizona, Tucson, Arizona 85721‐0077, USA;3. Lunar and Planetary Institute, 3600 Bay Area Blvd., Houston, Texas 77058, USA |
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| Abstract: | Abstract— 40Ar‐39Ar analyses of a total of 26 samples from eight shock‐darkened impact melt breccias of H‐chondrite affinity (Gao‐Guenie, LAP 02240, LAP 03922, LAP 031125, LAP 031173, LAP 031308, NWA 2058, and Ourique) are reported. These appear to record impacts ranging in time from 303 ± 56 Ma (Gao‐Guenie) to 4360 ± 120 Ma (Ourique) ago. Three record impacts 300–400 Ma ago, while two others record impacts 3900–4000 Ma ago. Combining these with other impact ages from H chondrites in the literature, it appears that H chondrites record impacts in the first 100 Ma of solar system history, during the era of the “lunar cataclysm” and shortly thereafter (3500–4000 Ma ago), one or more impacts ?300 Ma ago, and perhaps an impact ?500 Ma ago (near the time of the L chondrite parent body disruption). Records of impacts on the H chondrite parent body are rare or absent between the era of planetary accretion and the “lunar cataclysm” (4400‐4050 Ma), during the long stretch between heavy bombardment and recent breakup events (3500‐1000 Ma), or at the time of final breakup into meteorite‐sized bodies (<50 Ma). |
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