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Name: Witherite RRUFF ID: R050148 Ideal Chemistry: Ba(CO3) Locality: Settlingstones mine, Fourstones, Northumberland, England Source: Jim McGlasson Owner: RRUFF Description: Tan colored crystal fragment Status: The identification of this mineral has been confirmed by X-ray diffraction and chemical analysis |
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Mineral Group: [ Aragonite (18) ] | ||
Quick search: [ All Witherite samples (3) ] |
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: | R050148.1 | |||||||
Sample Description: | Powder | |||||||
Cell Refinement Output: |
a: 5.3048(3)Å b: 8.8854(2)Å c: 6.4216(4)Å alpha: 90.° beta: 90.° gamma: 90.° Volume: 302.68(2)Å3 Crystal System: orthorhombic |
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REFERENCES for Witherite | |
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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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Withering W, Kirwan R (1784) Experiments and observations on the terra ponderosa, Philosophical Transactions of the Royal Society of London, 74, 293-311 [view file] |
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Hoffmann C A S (1789) Mineralsystem des Herrn Inspektor Werners mit dessen Erlaubnis herausgegeben von C A S Hoffmann, Bergmannisches Journal, 1, 369-398 [view file] |
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Klaproth M H (1797) Noch einige Erfahrungen über Witherit und Strontianit, Beiträge zur Chemischen Kenntniss der Mineralkörper, 2, 84-91 [view file] |
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Zachariasen W H (1928) Untersuchungen über die Kristallstruktur von Sesquioxyden und Verbindungen ABO3, Skrifter Utgitt av Det Norske Videnskaps-Akademi i Oslo, 1, 1-165 [view file] |
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De Villiers J P R (1971) Crystal structures of aragonite, strontianite, and witherite, American Mineralogist, 56, 758-772 [view file] |
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Blount C (1974) Synthesis of barite, celestite, anglesite, witherite, and strontianite from aqueous solutions, American Mineralogist, 59, 1209-1219 [view file] |
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Chamberlain S C, Dossert W P, Siegel D I (1986) A new paragenesis and new localities for witherite, The Canadian Mineralogist, 24, 79-90 [view file] |
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Cloots R (1991) Raman spectrum of carbonates MIICO3 in the 1100-1000 cm-1 region: observation of the v1 mode of the isotopic (C16O218O)2- ion, Spectrochimica Acta Part A-Molecular and Biomolecular Spectroscopy, 47, 1745-1750 |
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Antao S M, Hassan I (2007) BaCO3: high-temperature crystal structures and the Pmcn R3m phase transition at 811°C, Physics and Chemistry of Minerals, 34, 573-580 |
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Antao S M, Hassan I (2009) The orthorhombic structure of CaCO3, SrCO3, PbCO3 and BaCO3: Linear structural trends, The Canadian Mineralogist, 47, 1245-1255 [view file] |
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Buzgar N, Apopei A I (2009) The Raman study of certain carbonates, Analele Stiintifice Ale Universitatii, Al. I. Cuza Iasi Geologie, 55, 97-112 [view file] |
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Ye Y, Smyth J R, Boni P (2012) Crystal structure and thermal expansion of aragonite-group carbonates by single-crystal X-ray diffraction, American Mineralogist, 97, 707-712 [view file] |
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Nie S, Liu Y, Liu Q, Wang M, Wang H (2017) Phase transitions and thermal expansion of BaCO3 and SrCO3 up to 1413 K, European Journal of Mineralogy, 29, 433-443 |
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Lindner M, Jordan G (2018) On the growth of witherite and its relacement by the Mg-bearing double carbonate norsethite: Implications for the dolomite problem, American Mineralogist, 103, 252-259 |
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Li K, Liu X, Guo R, Wu C, Peng B, Li Z, Duan X, Zhou Y, Pei C (2020) Non-isodiametric growth and confinement effect in the mineralisation of witherite, Mineralogical Magazine, 84, 524-532 |
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