Dodd, R. T. (1969) Petrofabric analysis of a large microporphyritic chondrule in the Parnallee meteorite. Mineralogical Magazine, 37 (286) 230-237 doi:10.1180/minmag.1969.037.286.10
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Petrofabric analysis of a large microporphyritic chondrule in the Parnallee meteorite | ||
| Journal | Mineralogical Magazine | ||
| Authors | Dodd, R. T. | Author | |
| Year | 1969 (June) | Volume | 37 |
| Issue | 286 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_37/37-286-230.pdf+ | ||
| DOI | doi:10.1180/minmag.1969.037.286.10Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 6259 | Long-form Identifier | mindat:1:5:6259:0 |
| GUID | 0 | ||
| Full Reference | Dodd, R. T. (1969) Petrofabric analysis of a large microporphyritic chondrule in the Parnallee meteorite. Mineralogical Magazine, 37 (286) 230-237 doi:10.1180/minmag.1969.037.286.10 | ||
| Plain Text | Dodd, R. T. (1969) Petrofabric analysis of a large microporphyritic chondrule in the Parnallee meteorite. Mineralogical Magazine, 37 (286) 230-237 doi:10.1180/minmag.1969.037.286.10 | ||
| In | (1969, June) Mineralogical Magazine Vol. 37 (286) Mineralogical Society | ||
| Abstract/Notes | SummaryOlivine microphenocrysts in a large microporphyritic chondrule in the Parnallee chondrite show a linear preferred orientation of the long (β = c) axes, which is thought to reflect flowage of a partly crystalline parent magma. The orientation pattern is somewhat disturbed by post-crystallization fracturing. | ||
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