NATROLEMOYNITE, A NEW HYDRATED SODIUM ZIRCONOSILICATE FROM MONT SAINT-HILAIRE, QUEBEC: DESCRIPTION AND STRUCTURE DETERMINATION

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Natrolemoynite is a new member of the lemoynite group found in altered or unaltered pegmatites cutting nepheline syenite at the Poudrette quarry, Mont Saint-Hilaire, Quebec. In altered pegmatites, it is associated with microcline, lemoynite, lepidocro cite, galena, sphalerite, calcite and pyrite, and in unaltered pegmatites, with biotite, microcline, albite, magnetite, a chlorite-gr oup mineral, a burbankite-group mineral, an unidentified donnayite-(Y)-like mineral, zircon and pyrochlore. Crystals are colorless to white (occasionally with a slightly pink to red tinge), bladed to prismatic, elongate along [001], with maximum widths of 1 mm and lengths of 2 mm. The mineral typically develops in compact radial aggregates and spheres 4 mm in maximum diameter. It is transparent to translucent, with a vitreous to subadamantine luster and a white streak. The Mohs hardness is 3. Perfect {100} a nd

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Acute appendicitis: sonographic criteria based on 250 cases.
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Two hundred and fifty consecutive patients with suspected appendicitis were examined with graded compression sonography. The initial diagnostic criterion for appendicitis was visualization of a noncompressible appendix; this was later modified to include the dimensions of the visualized appendix. The appendix was visualized in 91 of 250 patients (36%). Five adult patients with sonographically visible appendixes that were 6 mm or less in maximal diameter had either benign clinical follow-up (three patients) or a histologically normal appendix removed at surgery (two patients). However, two patients with appendixes measuring 6 mm in diameter and multiple appendicoliths had surgically confirmed acute appendicitis. Of 84 patients with visible appendixes measuring greater than 6 mm in maximal diameter, 78 had surgically confirmed acute appendicitis. In the remaining six, symptoms resolved spontaneously, and no surgery was required. In the absence of compelling clinical findings or an appendicolith, adult patients with maximal appendiceal diameters of 6 mm or less should undergo a period of close observation rather than immediate surgery. A diagnosis of appendicitis can be made in adult patients with persistent right lower quadrant pain and a visualized appendix greater than 6 mm in diameter.

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  • 10.2138/am-1997-11-1220
Lukechangite-(Ce), a new rare-earth-fluorocarbonate mineral from Mont Saint-Hilaire, Quebec
  • Dec 1, 1997
  • American Mineralogist
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Other| December 01, 1997 Lukechangite-(Ce), a new rare-earth-fluorocarbonate mineral from Mont Saint-Hilaire, Quebec Joel D. Grice; Joel D. Grice Canadian Museum of Nature, Research Division, Ottawa, ON, Canada Search for other works by this author on: GSW Google Scholar George Y. Chao George Y. Chao Carleton University, Canada Search for other works by this author on: GSW Google Scholar American Mineralogist (1997) 82 (11-12): 1255–1260. https://doi.org/10.2138/am-1997-11-1220 Article history first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Joel D. Grice, George Y. Chao; Lukechangite-(Ce), a new rare-earth-fluorocarbonate mineral from Mont Saint-Hilaire, Quebec. American Mineralogist 1997;; 82 (11-12): 1255–1260. doi: https://doi.org/10.2138/am-1997-11-1220 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu nav search search input Search input auto suggest search filter All ContentBy SocietyAmerican Mineralogist Search Advanced Search Abstract Lukechangite-(Ce), ideally Na3Ce2(CO3)4F, is a new mineral from Mont Saint-Hilaire, Quebec. It occurs as tabular, short prismatic, and barrel-shaped crystals up to 1 mm. It is colorless to pale beige with a white streak and a vitreous, or somewhat pearly on {0001}, luster. Associated minerals include microcline, analcime, sodalite, aegirine, serandite, eudialyte, catapleiite, fluorite, petersenite-(Ce), siderite, astrophyllite, and albite. Lukechangite-(Ce) is soft, Mohs hardness ≈ 4½, brittle, with an uneven to conchoidal fracture, and with perfect {0001} cleavage. Lukechangite-(Ce) is uniaxial negative, ω = 1.728(3) and ϵ = 1.542(1). It is hexagonal, space group P63/mmc, a = 5.068(1), c = 22.87(5) Å, V = 509(1) Å3, and Z = 2. The strongest X-ray powder diffraction lines [d (Å), I, hkl] are: 5.71(50)(004), 4.31(100)(101), 3.804(50)(006), 3.169(70)(105), 2.877(60)(106), 2.534(70)(110), 2.192(90B)(109,200,201), 1.978(70)(205), and 1.658(50)(209,210,211). An average of the electron-microprobe analyses gave Na2O 14.94, CaO 0.10, SrO 0.12, La2O3 16.36, Ce2O3 29.48, Pr2O3 1.95, Nd2O3 5.88, F 3.58, CO2 (28.40), and O ≡ F – 1.51, total 99.30 wt%. CO2 was calculated by stoichiometry from the results of the crystal-structure analysis. Dcalc is 4.02 g/cm3. The atomic arrangement of lukechangite-(Ce) has been refined to R = 3.4%. The structure is layered parallel to (001), with CO3 groups oriented parallel to the layering forming thick slabs incorporating either Ce or Na cations and a separate Na-F layer. The structure of lukechangite-(Ce) resembles that of huanghoite-(Ce) and baiyuneboite-(Ce) and is isostructural with synthetic Na3La2(CO3)4F. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article.

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Endovascular treatment of ruptured very small intracranial aneurysms with relatively wide - neck
  • Jul 28, 2010
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FERROKENTBROOKSITE, A NEW MEMBER OF THE EUDIALYTE GROUP FROM MONT SAINT-HILAIRE, QUEBEC, CANADA
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  • Journal of the American Academy of Dermatology
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  • 10.1016/0190-9622(92)70236-9
Small-diameter malignant melanoma: A common diagnosis in New South Wales, Australia
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Small diameter malignant melanoma
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  • Aug 10, 2013
  • Chinese journal of radiology
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  • Abstract
  • 10.1016/j.jvs.2022.07.163
Risk of Rupture and All Cause Mortality of Abdominal Aortic Ectasia: A Systematic Review and Meta-Analysis
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  • Journal of Vascular Surgery
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  • Cite Count Icon 76
  • 10.1007/s00268-001-0271-5
Lymph node staging of esophageal squamous cell carcinoma in patients with and without neoadjuvant radiochemotherapy: histomorphologic analysis.
  • May 1, 2002
  • World Journal of Surgery
  • Wolfgang Schröder + 5 more

In patients with squamous cell carcinoma of the esophagus, the preoperative clinical staging of the N category is primarily based on the lymph node size. Lymph nodes > 10 mm are considered to be tumor-infiltrated. This histopathologic study investigated the correlation of lymph node size and metastatic infiltration in esophageal carcinoma of patients with and without neoadjuvant radiochemotherapy. The specimens of 40 patients with squamous cell carcinoma of the esophagus were included in a prospective morphometric study. Half of these patients (n = 20) received preoperative radiochemotherapy. The number of resected lymph nodes were counted, and the largest diameter of each node was measured. Metastatic involvement of each node was analyzed by histologic examination. The frequency of lymph node metastases was calculated and correlated to the lymph node size. A total of 1196 lymph nodes with an average of 29.9 nodes per patient were resected and analyzed; 129 lymph nodes (10.8%) showed metastatic infiltration. The average size of 1067 tumor-free lymph nodes was 5.1 +/- 3.8 mm in maximum diameter, whereas the average size of 129 metastatic lymph nodes was 6.7 +/- 4.2 mm (p = 0.00006). Of all resected lymph nodes, 761 (63.6%) were < or = 5 mm in maximum diameter. Only 9.3% (n = 111) of all resected lymph nodes were > 10 mm in maximum diameter. There was no significant correlation between lymph node size and the frequency of nodal metastases. No difference in size could be demonstrated between patients with and without neoadjuvant radiochemotherapy. Diagnostic imaging techniques using size as the criterion of nodal infiltration cannot exactly assess the nodal status of patients with esophageal carcinoma. This is also true for patients after neoadjuvant radiochemotherapy. Therefore, evaluation of the nodal status in patients with squamous cell carcinoma of the esophagus is entirely based on pathohistologic analysis after a well defined lymphadenectomy.

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  • 10.2113/gscanmin.38.6.1457
ADAMSITE-(Y), A NEW SODIUM YTTRIUM CARBONATE MINERAL SPECIES FROM MONT SAINT-HILAIRE, QUEBEC
  • Dec 1, 2000
  • The Canadian Mineralogist
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  • 10.3749/canmin.48.2.267
ROGERMITCHELLITE, Na12(Sr,Na)24Ba4Zr26Si78(B,Si)12O246(OH)24{middle dot}18H2O, A NEW MINERAL SPECIES FROM MONT SAINT-HILAIRE, QUEBEC: DESCRIPTION, STRUCTURE DETERMINATION AND RELATIONSHIP WITH HFSE-BEARING CYCLOSILICATES
  • Apr 1, 2010
  • The Canadian Mineralogist
  • A M Mcdonald + 1 more

Rogermitchellite is a new, complex species of zirconosilicate found in igneous breccia at the Poudrette quarry, Mont Saint-Hilaire, Quebec. It is associated with aegirine, annite, galena, a labuntsovite-group mineral, manganoneptunite, microcline, pyrrhotite, sodalite and zircon. Paragenetically, the mineral crystallizes after aegirine and before microcline. Isolated, single crystals are colorless to grey, prismatic along [001], and slightly flattened perpendicular to this direction, with a maximum dimension of 0.1 × 0.25 mm. It develops as euhedral crystals displaying the prominent forms prism {100} and pinacoid {001}, with a minor, very shallow ditrigonal scalenohedron {10 l }. The mineral is transparent with a vitreous luster and a white streak and is non-luminescent. The Mohs hardness is 5, and no cleavage is evident. It is brittle with a conchoidal to splintery fracture. The calculated density is 3.34 g/cm 3 . Rogermitchellite is non-pleochroic, uniaxial positive, with ω 1.640(1) and e 1.663(1). Four analyses made on one crystal gave, as an average: Na 2 O 3.45, CaO 0.10, SrO 18.54, BaO 5.18, B 2 O 3 (calc.) 2.34, SiO 2 39.12, ZrO 2 26.39, TiO 2 0.63 and H 2 O (calc.) 6.96, for a total of 102.71 wt.%. The empirical formula, based on 288 anions and the sum of (Si + B) = 90 apfu , is: Na 12 (Sr 21.16 Na 1.17 Ca 0.21 ) ∑22.54 Ba 4.00 (Zr 25.33 Ti 0.93 ) ∑26.26 (Si 77.02 B 0.98 ) ∑78 B 12 O 246 (OH) 24 ·18H 2 O or, ideally, Na 12 Sr 24 Ba 4 Zr 26 Si 78 B 12 O 246 (OH) 24 ·18H 2 O. The mineral is trigonal, space group P 3 c 1, a 26.509(4), c 9.975(2) A, V 6070.6(1) A 3 and Z = 1. The strongest six lines on the X-ray powder-diffraction pattern [ d in A(I)( hkl )] are: 2.760(100)(442), 3.761(90)(402), 1.991(70)(444), 3.150(50)(441), 5.762(40)(400) and 3.924(30)(312). The crystal structure was refined to R = 4.62% and w R 2 = 12.73% for 1588 reflections [ F o > 4σ( F o )]. It consists of pairs (Si 3 O 9 ) rings (offset 30° relative to one another along [001]) linked to isolated ZrO 6 octahedra in a motif similar to that in benitoite. Additional (Si 3 O 9 ) and [Si 2 BO 7 (OH) 2 ] rings along with ZrO 6 octahedra complete a three-dimensional heteropolyhedral framework. Channels along [001] within this framework are occupied by Ba, Na, (Sr + Na) and H 2 O. Rogermitchellite has chemical and crystal-structure features common to benitoite, wadeite and catapleiite, and should be considered as a structural hybrid of these minerals. It possesses additional features (presence of essential B, Sr, H 2 O; trigonal symmetry) that make it unique.

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