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The relatively well-preserved ancient crust of Mars provides a natural window into early planetary evolution not available on Earth due to sustained tectonic recycling and erosion on this planet. Mars has generally been considered a one-plate, basalt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e5c9a3661167ce25f1b0751aa4f5de7
https://doi.org/10.21203/rs.3.rs-2359881/v1
https://doi.org/10.21203/rs.3.rs-2359881/v1
Publikováno v:
Journal of Geophysical Research: Planets. 128