作者: B. Bultel , C. Quantin-Nataf , M. Andréani , H. Clénet , L. Lozac’h
DOI: 10.1016/J.ICARUS.2015.06.037
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摘要: Abstract Recent investigations of alteration martian crustal outcrops suggest putative hydrothermal systems, which are favorable environments for the emergence life. In this study, we perform an analysis CRISM targeted observations covering in region between Hellas and Isidis basins with goal investigating phases. Over wide studied region, detect presence possible serpentines, chlorites, smectites carbonates. These detections occur within ejecta blankets, crater walls central uplifts impact craters. We investigate relation observed associations minerals ages craters assessed by count. No clear is observed. also relationship group detected mineral pre-impact depth from size This method allows us to reconstruct cross-section. that first 7 km crust may have undergone processes.