Adding Dimensions to the Lunar Geologic Map Using GIS

Mathematics – Logic

Scientific paper

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Geographic Information System, Iron Oxide, Light Plains, Titanium Dioxide

Scientific paper

We are applying Geographic Information Systems (GIS) technology to assemble a variety of lunar data types into one integrated database. The resulting combination of data will allow us to examine lunar geologic issues from a completely new perspective. To show the utility of GIS, we investigated the light plains deposits found on 4-7% of the nearside. The nature and origin of light plains have been a long-standing problem in lunar geology. Ideas for their origin include: true volcanic light plains, plains containing much impact melt, and emplacement of ejecta from basin-forming impacts. We made a spatial comparison between FeO and TiO2 derived from multispectral data acquired during the Galileo lunar flyby and digitized areas of light plains in their currently accepted locations. The chemical database provides an additional criteria for classifying the light plains regions. We have found that there are large variations in the FeO and TiO2 contents of the light plains. These units vary from relatively low FeO (6-8 wt.%) and low TiO2 (0.1 wt.%) to relatively high FeO (11-14 wt.%) and TiO2 (0.7-1.5 wt.%).

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