Constraints on the composition and petrogenesis of the Martian crust

Author:

McSween Harry Y.1,Grove Timothy L.2,Wyatt Michael B.3

Affiliation:

1. Department of Earth and Planetary Sciences; University of Tennessee; Knoxville Tennessee USA

2. Department of Earth, Atmospheric and Planetary Sciences; Massachusetts Institute of Technology; Cambridge Massachusetts USA

3. Department of Geological Sciences; Arizona State University; Tempe Arizona USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference126 articles.

1. Petrology of the Nandewar Volcano, N.S.W., Australia;Abbott;Contrib. Mineral. Petrol.,1969

2. A 4-Ga shock age for a Martian meteorite and implications for the cratering history of Mars;Ash;Nature,1996

3. Baker , V. R. S. Maruyama J. M. Dohm A theory for the geological evolution of Mars and related synthesis (GEOMARS) Lunar Planet. Sci. XXXIII 2002

4. Rheology of a long lava flow at Pavonis Mons, Mars;Baloga;J. Geophys. Res.,2003

5. Global mineral distributions on Mars;Bandfield;J. Geophys. Res.,2002

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