Reply to comment: “The Nakhla Martian meteorite is a cumulate igneous rock” by A. Treiman.
Autor: | Varela, M. E.1 evarela@criba.edu.ar, Kurat, G.2 kurat@univie.ac.at, Clocchiatti, R.3 clocchiatti@nimitz.saclay.cea.fr |
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Zdroj: | Mineralogy & Petrology. Feb2003, Vol. 77 Issue 3/4, p279-285. 7p. 1 Color Photograph. |
Databáze: | Academic Search Ultimate |
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