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Name: Graftonite RRUFF ID: R070153 Ideal Chemistry: (Fe2+,Mn2+,Ca)3(PO4)2 Locality: Bull Moose mine, Custer, Custer County, South Dakota, USA Source: James Shigley [view label] Owner: RRUFF Description: Dark brown vitreous massive Status: The identification of this mineral has only been confirmed by single-crystal X-ray diffraction. |
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| POWDER DIFFRACTION | |||||||
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| RRUFF ID: | R070153.9 | ||||||
| Sample Description: | Single crystal, powder profile is calculated | ||||||
| Cell Refinement Output: |
a: 8.8076(7)Å b: 11.556(2)Å c: 6.1396(7)Å alpha: 90° beta: 99.286(7)° gamma: 90° Volume: 616.7(2) Crystal System: monoclinic |
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| REFERENCES for Graftonite | |
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American Mineralogist Crystal Structure Database Record: [view record] |
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Anthony J W, Bideaux R A, Bladh K W, and Nichols M C (1990) Handbook of Mineralogy, Mineral Data Publishing, Tucson Arizona, USA, by permission of the Mineralogical Society of America. [view file] |
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Penfield S L (1900) On graftonite, a new mineral from Grafton, New Hampshire, and its intergrowth with triphylite, The American Journal of Science, 159, 20-32 [view file] |
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Lindberg M L (1950) Arrojadite, hühnerkobelite, and graftonite, American Mineralogist, 35, 59-76 [view file] |
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Calvo C (1968) The crystal structure of graftonite, American Mineralogist, 53, 742-750 [view file] |
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Hurlbut C S, Aristarain L F (1968) Beusite, a new mineral from Argentina, and the graftonite-beusite series, American Mineralogist, 53, 1799-1814 [view file] |
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Fransolet A M (1977) Intercroissances et inclusions dans les associations graftonite-sarcopside-triphylite, Bulletin de la Société Française de Minéralogie et de Cristallographie, 100, 198-207 |
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Cerný P, Selway J B, Ercit T S, Breaks F W, Anderson A J, Anderson S D (1998) Graftonite beusite in granitic pegmatites of the Superior Province: a study in contrasts, The Canadian Mineralogist, 36, 367-376 [view file] |
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Smeds S A, Uher P, Cerný P, Wise M A, Gustafsson L, Penner P (1998) Graftonite beusite in Sweden: primary phases, products of exsolution, and distribution in zoned populations of granitic pegmatites, The Canadian Mineralogist, 36, 377-394 [view file] |
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