Shelley, D. (1967) Myrmekite and myrmekite-like intergrowths. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (280) 491-503 doi:10.1180/minmag.1967.036.280.03
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Myrmekite and myrmekite-like intergrowths | ||
| Journal | Mineralogical Magazine and Journal of the Mineralogical Society | ||
| Authors | Shelley, D. | Author | |
| Year | 1967 (December) | Volume | 36 |
| Issue | 280 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-280-491.pdf+ | ||
| DOI | doi:10.1180/minmag.1967.036.280.03Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 6111 | Long-form Identifier | mindat:1:5:6111:1 |
| GUID | 0 | ||
| Full Reference | Shelley, D. (1967) Myrmekite and myrmekite-like intergrowths. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (280) 491-503 doi:10.1180/minmag.1967.036.280.03 | ||
| Plain Text | Shelley, D. (1967) Myrmekite and myrmekite-like intergrowths. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (280) 491-503 doi:10.1180/minmag.1967.036.280.03 | ||
| In | (1966) Mineralogical Magazine Vol. 36 (280) Mineralogical Society | ||
| Abstract/Notes | SummaryMyrmekite-like intergrowths in the Lewisian gneiss and the igneous complex of Loch Borolan are described. The intergrowths are of diverse mineral composition but have many features in common with myrmekite and it is shown that they result from the constriction of a previously existing mineral during the growth, in the solid state, of the host mineral. More than one stage of intergrowth is often found and these stages can be correlated with geological events. | ||
See Also
These are possibly similar items as determined by title/reference text matching only.
 | |
 | |
 | |
 | |
 | |
 | |
 | |
 | |
 | |
 | |
 |