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Name: Antigorite RRUFF ID: R070228 Ideal Chemistry: Mg3Si2O5(OH)4 Locality: Wood's Chrome Mine (Wood's Mine), Texas, Lancaster County, Pennsylvania, USA Source: Michael Scott S100701 [view label] Owner: RRUFF Description: Compact massive, light to dark green associated with chromite Status: The identification of this mineral has been confirmed by X-ray diffraction and chemical analysis |
Mineral Groups: [ serpentine (12) ] [ Clay (86) ] |
CHEMISTRY | ||||||||||
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RAMAN SPECTRUM | ||||||||||||
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BROAD SCAN WITH SPECTRAL ARTIFACTS | ||||||||||||
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INFRARED SPECTRUM (Attenuated Total Reflectance) | |||||||||||||||
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POWDER DIFFRACTION | ||||||||
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RRUFF ID: | R070228.1 | |||||||
Sample Description: | Powder | |||||||
Cell Refinement Output: |
a: 43.617(3)Å b: 9.208(1)Å c: 7.2716(4)Å alpha: 90° beta: 92.34(1)° gamma: 90° Volume: 2918.1(3)Å3 Crystal System: monoclinic |
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REFERENCES for Antigorite | |
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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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Schweizer E (1840) Ueber den Antigorit, ein neues Mineral, Annalen der Physik und Chemie, 19, 595-599 [view file] |
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Zussman J (1954) Investigation of the crystal structure of antigorite, Mineralogical Magazine, 30, 498-512 [view file] |
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Zussman J, Brindley G W, Comer J J (1957) Electron diffraction studies of serpentine minerals, American Mineralogist, 42, 133-153 [view file] |
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International Mineralogical Association (1967) Commission on new minerals and mineral names, Mineralogical Magazine, 36, 131-136 [view file] |
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Bish D L, Brindley G W (1978) Deweylites, mixtures of poorly crystalline hydrous serpentine and talc-like minerals, Mineralogical Magazine, 42, 75-84 [view file] |
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Leake B E (1978) Nomenclature of amphiboles, American Mineralogist, 63, 1023-1052 [view file] |
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Dungan M A (1979) A microprobe study of antigorite and some serpentine pseudomorphs, The Canadian Mineralogist, 17, 771-784 [view file] |
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Veblen D R, Buseck P R (1979) Serpentine minerals: Intergrowth and new combination structures, Science, 206, 1398-1400 [view file] |
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Yada K (1979) Microstructures of chrysotile and antigorite by highresolution electron microscopy, The Canadian Mineralogist, 17, 679-691 [view file] |
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Zussman J (1987) Minerals and the electron microscope, Mineralogical Magazine, 51, 129-138 [view file] |
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Otten M T (1993) High-resolution transmission electron microscopy of polysomatism and stacking defects in antigorite, American Mineralogist, 78, 75-84 [view file] |
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Uehara S, Kamata K (1994) Antigorite with a large supercell from Saganoseki, Oita Prefecture, Japan, The Canadian Mineralogist, 32, 93-103 [view file] |
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O'Hanley D S, Wicks F J (1995) Conditions of formation of lizardite, chrysotile and antigorite, Cassiar, British Columbia, The Canadian Mineralogist, 33, 753-773 [view file] |
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Uehara S (1998) TEM and XRD study of antigorite and superstructures, The Canadian Mineralogist, 36, 1595-1605 [view file] |
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Dódony I, Pósfai M, Buseck P R (2002) Revised structure models for antigorite: An HRTEM study, American Mineralogist, 87, 1443-1457 [view file] |
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Rinaudo C, Gastaldi D, Belluso E (2003) Characterization of chrysotile, antigorite and lizardite by FT-Raman spectroscopy, The Canadian Mineralogist, 41, 883-890 [view file] |
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Capitani G C, Mellini M (2006) The crystal structure of a second antigorite polysome (m = 16), by single-crystal synchrotron diffraction, American Mineralogist, 91, 394-399 [view file] |
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Dódony I, Pósfai M, Buseck P R (2006) Does antigorite really contain 4- and 8-membered rings of tetrahedra?, American Mineralogist, 91, 1831-1838 [view file] |
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Capitani G C, Mellini M (2007) High-resolution transmission electron microscopy (HRTEM) investigation of antigorite polysomes (m = 15 to 18), American Mineralogist, 92, 64-71 [view file] |
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Roth P (2007) Antigorite, in Minerals first discovered in Switzerland and minerals named after Swiss individuals Kristallografik Verlag Achberg Germany 34-35 |
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Noguchi N, Moriwaki T, Ikemoto Y, Shinoda K (2012) OH group behavior and pressure-induced amorphization of antigorite examined under high pressure and temperature using synchrotron infrared spectrscopy, American Mineralogist, 97, 134-142 [view file] |
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Krivovichev S V (2013) Structural complexity of minerals: information storage and processing in the mineral world, Mineralogical Magazine, 77, 275-326 |
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Marquardt H, Speziale S, Koch-Müller M, Marquardt K, Capitani G C (2015) Structural insights and elasticity of single-crystal antigorite from high-pressure Raman and Brillouin spectroscopy measured in the (010) plane, American Mineralogist, 100, 1932-1939 |
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Clément M, Padrón-Navarta J A, Tommasi A, Mainprice D (2018) Non-hydrostatic stress field orientation inferred from orthopyroxene (Pbca) to low-clinoenstatite (P21/c) inversion in partially dehydrated serpentinites, American Mineralogist, 103, 993-1001 |
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Queffelec A, Fouéré P, Paris C, Stouvenot C, Bellot-Gurlet L (2018) Local production and long-distance procurement of beads and pendants with high mineralogical diversity in an early Saladoid settlement of Guadeloupe (French West Indies), Journal of Archaeological Science: Reports, 21, 275-288 |
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Di Perro S, Groppo C, Compagnoni R, Capitani G, Mellini M (2019) Fe-rich antigorite: a rock-forming mineral from low-temperature/high-pressure meta-ophicarbonates, European Journal of Mineralogy, 31, 775-784 |
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Ferrand T P (2019) Neither antigorite nor its dehydration is "metastable", American Mineralogist, 104, 788-790 |
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Shen T, Zhang C, Chen J, Hermann J, Zhang L, Pardón-Navarta J A, Chen L, Xu J, Yang J (2020) Changes in the cell parameters of antigorite close to its dehydration reaction at subduction zone conditions, American Mineralogist, 105, 569-582 |
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