Planetary Geologic Mappers 2021 (LPI Contrib. No. 2610) 7045.pdf From morpho-stratigraphic to geo(spectro)-stratigraphic units: the PLANMAP contribution. Matteo Massironi1, Angelo Pio Rossi2, Jack Wright3, Francesca Zambon4, Claudia Poehler5, Lorenza Giacomini4, Cristian Carli4, Sabrina Ferrari6, Andrea Semenzato7, Erica Luzzi2, Riccardo Pozzobon6, Gloria Tognon6, David A. Rothery3, Carolyn Van der Bogert5, V. Galluzzi4, Francesca Altieri4 1Department of Geosciences, University of Padova,
[email protected], 2Jacobs University Bremen, 3Open University, 4INAF-IAPS, 5Westfälische-Wilhelms Universität Münster 6CISAS, University of Padova 7Engineering Ingegneria Informatica S.p.A., Venezia Introduction: From the Apollo era onward, planetary ‘geologic’ mapping has been carried out using a photo-interpretative approach mainly on panchromatic and monochromatic images. This limits the definition of geological units to morpho-stratigraphic considerations so that units have been mainly defined by their stratigraphic position, surface textures and morphology, and attribution to general emplacement processes (a few related to magmatism, some broad sedimentary environments, some diverse impact domains, and all with uncertainties of interpretation). On the other hand, geological units on Earth are defined by several Figure 1: in-series interpretation from Giacomini et al. parameters besides the stratigraphic ones, such as rock EGU 2021-15052 textures, lithology, composition, and numerous environmental conditions of their origin (diverse Contextual interpretation: Geo(spectro)- magmatic, volcanic, metamorphic and sedimentary stratigraphic maps can be also produced directly from a environments). Hence, traditional morpho-stratigraphic contextual work on black and white images and RGB maps of planets and geological maps on the Earth are color compositions either using Principal Component still separated by an important conceptual and effective (PC) analysis (see Mercury examples in Semenzato et gap.