| Reference Type | Journal (article/letter/editorial) |
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| Title | Growth twinning in phacolite |
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| Journal | Mineralogical Magazine | ISSN | 0026-461X |
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| Authors | Akizuki, Mizuhiko | Author |
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| Konno, Hiroshi | Author |
| Year | 1987 (September) | Volume | 51 |
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| Issue | 361 |
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| Publisher | Mineralogical Society |
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| Download URL | https://rruff.info/doclib/MinMag/Volume_51/51-361-427.pdf+ |
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| DOI | doi:10.1180/minmag.1987.051.361.09Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 1402 | Long-form Identifier | mindat:1:5:1402:5 |
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| GUID | 0 |
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| Full Reference | Akizuki, Mizuhiko, Konno, Hiroshi (1987) Growth twinning in phacolite. Mineralogical Magazine, 51 (361) 427-430 doi:10.1180/minmag.1987.051.361.09 |
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| Plain Text | Akizuki, Mizuhiko, Konno, Hiroshi (1987) Growth twinning in phacolite. Mineralogical Magazine, 51 (361) 427-430 doi:10.1180/minmag.1987.051.361.09 |
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| In | (1987, September) Mineralogical Magazine Vol. 51 (361) Mineralogical Society |
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| Abstract/Notes | AbstractPhacolite from Mitaki, Sendai City, Japan, has a core of penetration-twinned chabazite. The crystal has a convex (0001) face on which many twin individuals are produced by a two-dimensional nucleation mechanism, resulting in complicated twinning during growth. Both the r and the faces repeat finely during growth because of twinning, resulting in {112Ì„3} sectors with polysynthetic twinning. Finally, single structures nucleate on the crystal edges [211Ì„] and develop along the (112Ì„3) face, penetrating each other near the centre of the face. |
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