Reference Type | Journal (article/letter/editorial) |
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Title | The Nakhla Martian meteorite is a cumulate igneous rock. Comment on "Glass-bearing inclusions in Nakhla (SNC meteorite) augite: heterogeneously trapped phases" (2001) by M. E. Varela, G. Kurat, and R. Clocchiatti |
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Journal | Mineralogy and Petrology |
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Authors | Treiman, A. H. | Author |
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Year | 2003 (February 1) | Volume | 77 |
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Issue | 3 |
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Publisher | Springer Science and Business Media LLC |
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DOI | doi:10.1007/s007100300000Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 16565 | Long-form Identifier | mindat:1:5:16565:7 |
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GUID | 0 |
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Full Reference | Treiman, A. H. (2003) The Nakhla Martian meteorite is a cumulate igneous rock. Comment on "Glass-bearing inclusions in Nakhla (SNC meteorite) augite: heterogeneously trapped phases" (2001) by M. E. Varela, G. Kurat, and R. Clocchiatti. Mineralogy and Petrology, 77 (3) 271-277 doi:10.1007/s007100300000 |
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Plain Text | Treiman, A. H. (2003) The Nakhla Martian meteorite is a cumulate igneous rock. Comment on "Glass-bearing inclusions in Nakhla (SNC meteorite) augite: heterogeneously trapped phases" (2001) by M. E. Varela, G. Kurat, and R. Clocchiatti. Mineralogy and Petrology, 77 (3) 271-277 doi:10.1007/s007100300000 |
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In | (2003, February) Mineralogy and Petrology Vol. 77 (3) Springer Science and Business Media LLC |
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