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Hawthorne, F. C., Ball, N. A., Nizamoff, J. W., Simmons, W. B. (2009) Zigrasite, MgZr(PO4)2(H2O)4, a new phosphate mineral from the Dunton Quarry, Newry, Oxford County, Maine, USA. Mineralogical Magazine, 73 (3) 415-420 doi:10.1180/minmag.2009.073.3.415

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Reference TypeJournal (article/letter/editorial)
TitleZigrasite, MgZr(PO4)2(H2O)4, a new phosphate mineral from the Dunton Quarry, Newry, Oxford County, Maine, USA
JournalMineralogical Magazine
AuthorsHawthorne, F. C.Author
Ball, N. A.Author
Nizamoff, J. W.Author
Simmons, W. B.Author
Year2009 (June)Volume73
Issue3
PublisherMineralogical Society
URL
Download URLhttps://rruff.info/rruff_1.0/uploads/MM73_415.pdf+
DOIdoi:10.1180/minmag.2009.073.3.415Search in ResearchGate
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Mindat Ref. ID16990450Long-form Identifiermindat:1:5:16990450:2
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Full ReferenceHawthorne, F. C., Ball, N. A., Nizamoff, J. W., Simmons, W. B. (2009) Zigrasite, MgZr(PO4)2(H2O)4, a new phosphate mineral from the Dunton Quarry, Newry, Oxford County, Maine, USA. Mineralogical Magazine, 73 (3) 415-420 doi:10.1180/minmag.2009.073.3.415
Plain TextHawthorne, F. C., Ball, N. A., Nizamoff, J. W., Simmons, W. B. (2009) Zigrasite, MgZr(PO4)2(H2O)4, a new phosphate mineral from the Dunton Quarry, Newry, Oxford County, Maine, USA. Mineralogical Magazine, 73 (3) 415-420 doi:10.1180/minmag.2009.073.3.415
In(2009, June) Mineralogical Magazine Vol. 73 (3) Mineralogical Society
Abstract/NotesZigrasite, ideally MgZr(PO4)2(H2O)4, is a new secondary phosphate mineral from the giant 1972 gem tourmaline-bearing pocket at the Dunton Quarry, Newry, Oxford County, Maine, USA. It occurs as subhedral blocky grains sometimes exceeding 1 mm in maximum dimension and perched on tourmaline. These grains are complex aggregates ofthree distinct phases, zigrasite and two unnamed phases: the Ca analogue of zigrasite, CaZr(PO4)2(H2O)4, and Zr(PO3OH)2(H2O)4. Zigrasite is associated with tourmaline, microcline, quartz, albite, beryl, amblygonite-montebrasite, childreniteeosphorite and apatite, and crystallized as one of the latest minerals during pocket formation. It is offwhite to pale yellow or light tan, translucent with a white streak and a vitreous lustre, and shows light blue to pale yellow cathodoluminescence. Mohs hardness is 3 and the measured and calculated densities are 2.76(4) and 2.66 g/cm3. The mineral has imperfect cleavage in two directions, parallel to (010) and (001), shows no parting, is brittle and has a hackly fracture. In transmitted light, it is colourless and non-pleochroic, biaxial negative with α 1.597(1), β 1.622 (1), γ 1.635 (1), with 2V(meas) = 65.5(4)º and 2V(calc.) = 71º. Zigrasite is triclinic, P , a 5.3049(2) Å, b 9.3372(4) Å, c 9.6282(5) Å, α 97.348(1)º, β 91.534(1)º, γ 90.512(4)º, V 472.79(5) Å3, Z = 2. The seven strongest lines in the X-ray powder diffraction pattern are as follows: d (Ê), I, (hkl): 9.550, 100, (001); 4.108, 70, ; 4.008, 50, (111); 4.589, 40, (110); 3.177, 40, (112); 3.569, 30, (0 2), 2.660, 30, (200),(11),(130); 3.273, 20, (12). Chemical analysis by electron microprobe gave P2O5 37.59, ZrO2 32.27, HfO2 0.34, FeO 0.20, MgO 10.37, ZnO 0.17, F 0.13, LOI 18.60, less O:F 0.05 = total 99.62 wt.%. The resulting empirical formula is (–)Σ=0.99(Zr0.99Hf0.01)Σ=1.00 P2.00O8(H2O)4 on the basis of12 O atoms with H2O = 4 per formula unit from crystal-structure analysis, and the end-member formula is MgZr(PO4)2(H2O)4.

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Dunton Gem Quarry, Newry, Oxford County, Maine, USA

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Zigrasite

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Dunton Gem Quarry, Newry, Oxford County, Maine, USA Zigrasite


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