Ground-based stratigraphic correlation of the Jura and Knockfarril Hill members of the Murray formation, Gale crater: bridging the Vera Rubin ridge – Glen Torridon divide
Résumé
Lithostratigraphic correlation representsa fundamental tool for interpreting the depositionalhistory and stratal architecture in sedimentaryrock successions. On Earth, this is accomplished bymeasuring the thickness and lithologies through a stratigraphicunit at multiple places along and across strike,then linking similar rock types. Across kilometer-scaledistances, such correlations have the potential to notonly connect lithologies, but also identify units thatwere deposited at or near the same time as a single bodyof sediment. Prior to the exploration of Gale crater byCuriosity, this type of correlation had not been possibleon Mars because of the requirement for making groundbasedobservations of the same unit in multiple locations.This paper reports on stratigraphic correlation ofthe Jura and Knockfarril Hill members of the Murrayformation across the Vera Rubin ridge (VRR) and GlenTorridon (GT) areas, which are separated by topographic,mineralogic, and spectral boundaries.
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