Abstract
The shatter cones found in the late 2000s in an area at least 3 km2 in extent 12 km northeast of Santa Fe, New Mexico, along with petrographic evidence of low shock-metamorphic levels indicate the presence of a so far unknown, deeply eroded impact structure that is between 300 Ma and 1 Ga in age and a minimum final crater diameter of ~6–13 km.
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References
Cavosie, A. J., & Lugo, C. (2014). Shocked apatite from the Santa Fe impact structure (USA): A new accessory mineral for studies of shock metamorphism. In 45th Lunar and Planetary Science Conference, abstract #1691.
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Fackelman, S. P., Morrow, J. R., Koeberl, C., & McElvain, T. H. (2008). Shatter cone and microscopic shock-alteration evidence for a post-Paleoproterozoic terrestrial impact structure near Santa Fe, New Mexico, USA. Earth and Planetary Science Letters, 270, 290–299.
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Flamini, E., Coletta, A., Battagliere, M.L., Virelli, M. (2019). Santa Fe, USA. In: Flamini, E., Di Martino, M., Coletta, A. (eds) Encyclopedic Atlas of Terrestrial Impact Craters. Springer, Cham. https://doi.org/10.1007/978-3-030-05451-9_167
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DOI: https://doi.org/10.1007/978-3-030-05451-9_167
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