Mathematics – Logic
Scientific paper
Sep 1982
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982apg..book..323l&link_type=abstract
In NASA, Washington Advan. in Planetary Geol. p 323-352 (SEE N83-12006 02-91)
Mathematics
Logic
Evolution (Development), Histories, Mercury (Planet), Moon, Planetary Geology, Geology, Igneous Rocks, Lunar Geology, Planetary Evolution, Tectonics
Scientific paper
To determine a planet's thermal history, a wide range of data is necessary. These data include remote sensing results, photogeologic evidence, magnetic field and remanent magnetization data, composition and ages of samples, and physical parameters of the planet and its orbit. Few of these data form unambiguous constraints for thermal models of Mercury. Igneous Chronology as the time history of the differentiation and igneous activity, is defined. Igneous Chronology is used here in the sense of the apparent igneous or relative chronology of geologic events, such as plains formation (through whatever mechanism) relative to the crater production and tectonic history (lineament and scarp formation).
No associations
LandOfFree
The intercrater plains of Mercury and the Moon: Their nature, origin and role in terrestrial planet evolution. Thermal histories of Mercury and the Moon does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with The intercrater plains of Mercury and the Moon: Their nature, origin and role in terrestrial planet evolution. Thermal histories of Mercury and the Moon, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and The intercrater plains of Mercury and the Moon: Their nature, origin and role in terrestrial planet evolution. Thermal histories of Mercury and the Moon will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1256889