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Autor:
Gilles Dromart, B. L. Ehlmann, Laetitia Le Deit, D. M. Rubin, Nicolas Mangold, Lauren A. Edgar, W. Rapin, K. E. Herkenhoff, Jay L. Dickson, Olivier Gasnault, R. C. Wiens, Stéphane Le Mouélic, Valerie Fox, Sylvestre Maurice
Introduction: Gale crater preserves a 5 km thick sequence of stratified rocks, the lower-most section of which exhibits orbital spectra signatures of clay minerals transitioning up to sulfates over several hundred meters of stratigraphy [1,2]. Unders
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::58c8ffd27017fe10379179456e917cbe
https://doi.org/10.5194/epsc2020-757
https://doi.org/10.5194/epsc2020-757
