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Fluorite crystal

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Journal Article
Journal: Economic Geology
Published: 01 January 1947
Economic Geology (1947) 42 (1): 78–82.
...William Stephens Twenhofel Abstract Temperature determinations made by heating liquid inclusions in a fluorite crystal from the Greenleaf no. 1 prospect, Fluorite Ridge, Luna County, New Mexico, indicate that the crystal started its growth at about 202 degrees C. and continued growth until...
Journal Article
Published: 01 April 1995
European Journal of Mineralogy (1995) 7 (2): 267–276.
Journal Article
Published: 01 December 1967
American Mineralogist (1967) 52 (11-12): 1735–1750.
...C. Ervin Brown Abstract Near Volga, Iowa, vugs lined with small but well-formed crystals of calcite, color-zoned fluorite, sphalerite, and pyrite are in the lowermost phosphatic sediments of the Maquo-keta Shale. The association of calcite, pyrite, and sphalerite and their paragenesis, crystal...
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(a) Fluorite crystal structure. (b) Cotunnite-type crystal structure. Green spheres represent the Th4+ cations, red spheres represent the O2– anions. (Color online.)
Published: 01 May 2018
Figure 1. ( a ) Fluorite crystal structure. ( b ) Cotunnite-type crystal structure. Green spheres represent the Th 4+ cations, red spheres represent the O 2– anions. (Color online.)
Image
Formation of cavities by laser ablation inside a fluorite crystal. a) Low magnification showing the microcracks around the ablation cavities inside a fluorite crystal. b and c) Microcracks connected with the surface of the crystal. d) Ablation cavity inside a fluorite crystal produced with a single laser shot of high energy; a microcrack connected to the cavity is visible. e) Interpretation schema showing the ablation cavity and the microcracks.
Published: 01 November 2000
Fig. 3. Formation of cavities by laser ablation inside a fluorite crystal. a) Low magnification showing the microcracks around the ablation cavities inside a fluorite crystal. b and c) Microcracks connected with the surface of the crystal. d) Ablation cavity inside a fluorite crystal produced
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Photomicrographs: a) Ablation cavity in a fluorite crystal not sealed after experiment (200°C, 4 weeks). Elongated inclusions are formed by healing of the microcracks. b) and c) Microphotographs of the same synthetic fluid inclusion in fluorite produced from an ablation cavity showing an elongation along the laser beam axis (oil immersion objective x100); b): top of the cavity with the visible vapour bubble; c): bottom of the cavity under the vapour phase. d) Pyramidal quartz overgrowths parallel to c axis perpendicular to prismatic face (300°C, 5 weeks). e) Healed microcracks in quartz with numerous flat inclusions. f) Inclusion in quartz made from an ablation cavity.
Published: 01 November 2000
Fig. 4. Photomicrographs: a) Ablation cavity in a fluorite crystal not sealed after experiment (200°C, 4 weeks). Elongated inclusions are formed by healing of the microcracks. b) and c) Microphotographs of the same synthetic fluid inclusion in fluorite produced from an ablation cavity showing
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—Fluorite crystal showing inclusions of hydrocarbons. Magnification 2X.
Published: 01 May 1937
FIG. 1. —Fluorite crystal showing inclusions of hydrocarbons. Magnification 2X.
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Published: 01 June 2005
TABLE 2. REE AND Y DATA ON YELLOW FLUORITE CRYSTALS FROM HYDROTHERMAL BARITE-FLUORITE VEINS FROM THE ERZGEBIRGE EASTERN GERMANY
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(a) Optical cathodoluminescence (OCL) images of fluorite crystals showing multiple dissolution, precipitation and brecciation events that are not visible using traditional optical microscopy. Samples from Sedling mine [NY8592241110] (ESE–WNW Quarter Point vein). (b) OCL images of calcite crystals showing zonal growth and brecciation, but lacking the obvious dissolution–precipitation textures seen in fluorite. Samples from Nenthead [NY7864442992] (ESE–WNW Quarter Point vein)..
Published: 11 March 2021
Fig. 10. ( a ) Optical cathodoluminescence (OCL) images of fluorite crystals showing multiple dissolution, precipitation and brecciation events that are not visible using traditional optical microscopy. Samples from Sedling mine [NY8592241110] (ESE–WNW Quarter Point vein). ( b ) OCL images
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Published: 01 June 2005
TABLE 1. SAMPLE LOCATIONS AND DESCRIPTIONS OF YELLOW FLUORITE CRYSTALS COLLECTED IN THE ERZGEBIRGE EASTERN GERMANY
Series: Special Publications of the Society of Economic Geologists
Published: 01 January 1996
DOI: 10.5382/SP.04.20
EISBN: 9781629490281
... Fluorspar District. The Okorusu ores consist of massive replacement fluorite and large fluorite crystals deposited in vugs. Purple and green replacement fluorite contains abundant finely crystallized inclusions of quartz, apatite, goethite, and calcite, together with minor strontianite, barite, rutile...
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Chondrite-normalized REE patterns of the yellow fluorite crystals. Normalization was performed using the chondrite data given by Anders & Grevesse (1989). Note that all samples are typified by patterns that are enriched in the MREE.
Published: 01 June 2005
F ig . 3. Chondrite-normalized REE patterns of the yellow fluorite crystals. Normalization was performed using the chondrite data given by Anders & Grevesse (1989) . Note that all samples are typified by patterns that are enriched in the MREE.
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Fluorite occurrences at Olympic Dam and in the Gawler silicic large igneous province (SLIP). A: Intergrown fluorite and chalcocite (opaque) crystals. Sample RD3449, 431.4 m, scale bar 100 μm. B: Fluorite daughter crystals in a melt inclusion hosted by a quartz phenocryst in the Gawler SLIP rhyolite. Sample GC8, scale bar 50 μm. C: Fluorite crystal in a quartz phenocryst in Gawler SLIP rhyolite. Sample GC15, scale bar 20 μm. D: Interstitial fluorite crystal in the Hiltaba Suite granite. Sample HS1, scale bar 500 μm.
Published: 01 November 2011
Figure 2. Fluorite occurrences at Olympic Dam and in the Gawler silicic large igneous province (SLIP). A: Intergrown fluorite and chalcocite (opaque) crystals. Sample RD3449, 431.4 m, scale bar 100 μm. B: Fluorite daughter crystals in a melt inclusion hosted by a quartz phenocryst in the Gawler
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Backscattered electron (BSE) images showing occurrence and mineral associations of zinconigerite-2N1S and -6N6S from the Xianghualing skarn. (a) Euhedral zinconigerite-2N1S crystals among fluorite crystals; (b) Zinconigerite-2N1S crystal veinlets among fluorite; (c and d) euhedral zinconigerite-6N6S crystals among fluorite crystals. Abbreviations: 2N1S = zinconigerite-2N1S; 6N6S = zinconigerite-6N6S; Fl = fluorite; Mgt = margarite; Chb = chrysoberyl; Plg = phlogopite.
Published: 03 October 2022
Figure 2. Backscattered electron (BSE) images showing occurrence and mineral associations of zinconigerite-2 N 1 S and -6 N 6 S from the Xianghualing skarn. ( a ) Euhedral zinconigerite-2 N 1 S crystals among fluorite crystals; ( b ) Zinconigerite-2 N 1 S crystal veinlets among fluorite; ( c
Journal Article
Published: 01 June 2005
The Canadian Mineralogist (2005) 43 (3): 883–898.
...TABLE 2. REE AND Y DATA ON YELLOW FLUORITE CRYSTALS FROM HYDROTHERMAL BARITE-FLUORITE VEINS FROM THE ERZGEBIRGE EASTERN GERMANY ...
FIGURES | View All (5)
Journal Article
Journal: Economic Geology
Published: 01 December 1984
Economic Geology (1984) 79 (8): 1833–1856.
... available transparent minerals in the paragenetic sequence: fluorite, sphalerite, quartz, calcite, and barite. The bulk of the fluid inclusion data, however, was from fluorite crystals.The fluorite crystals from the bedded replacement deposits are color banded. The banding sequence is observable...
Journal Article
Published: 01 July 2016
American Mineralogist (2016) 101 (7): 1604–1623.
... of fine-grained anatase as the sole Ti-oxide mineral, concentrically banded botryoidal fluorite textures, and presumed hydration of phosphate minerals. Fluid interaction with Ca-rich lithologies is known to initiate fluorite crystallization which may cause destabilization of (HREE,Ti,Nb)-fluoride...
FIGURES | View All (10)
Journal Article
Journal: GSA Bulletin
Published: 01 April 1965
GSA Bulletin (1965) 76 (4): 441–462.
... are generally: (1) wall zones of graphic granite; (2) outer-intermediate zones of biotite, cyrtolite, and perthite; (3) middle-intermediate zones of giant perthite crystals; and (4) inner-intermediate zones of euhedral fluorite crystals. Compromise surfaces between some minerals are interpreted as evidence...
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Examples of fluid inclusion assemblages (FIAs) containing primary fluid inclusions. (a) Photomicrograph of a portion of a quartz crystal from the epithermal Ag deposits at Guanajuato, Mexico, showing three primary FIAs outlining former growth surfaces in the crystal. (b) Photomicrograph of a portion of a quartz crystal from the epithermal Ag deposits at Guanajuato, Mexico, showing two FIAs: one (FIA 1) contained within a growth band in the crystal and the other (FIA 2) outlining the growth surface that terminates the growth band. These two FIAs likely represent one fluid event associated with growth of the quartz crystal. (c) Photomicrograph of a portion of a quartz vein from the Copper Creek, Arizona, porphyry prospect showing two FIAs (pFIA 1 and pFIA 2) containing primary inclusions along growth surfaces in the crystal and two FIAs (sFIA 3 and sFIA 4) containing secondary inclusions trapped along healed fractures in the quartz. (d) Photomicrograph of a portion of a quartz vein from the Marte porphyry-epithermal system, Chile, showing an FIA consisting of vapor-rich fluid inclusions. (e) Photomicrograph of a portion of a fluorite crystal from the Cave-in-Rock district, southern Illinois, showing an FIA consisting of primary, negative crystal-shaped inclusions that are contained within a single color-banded growth zone in the fluorite crystal. (f) Photomicrograph of a portion of a fluorite crystal from the Cave-in-Rock district, southern Illinois, showing an FIA consisting of primary, irregularly shaped inclusions that are all contained within a single growth band in the fluorite. Note that even though the inclusions are mostly irregularly shaped, they all homogenize at the same temperature (±1°C).
Published: 01 December 2018
trapped along healed fractures in the quartz. (d) Photomicrograph of a portion of a quartz vein from the Marte porphyry-epithermal system, Chile, showing an FIA consisting of vapor-rich fluid inclusions. (e) Photomicrograph of a portion of a fluorite crystal from the Cave-in-Rock district, southern
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Backscattered electron images showing (a) occurrence and mineral associations of chukochenite and (b) euhedral chukochenite crystals among fluorite crystals. Abbreviations: Ckc = chukochenite; Fl = fluorite; Na-M = Na-matgarite.
Published: 01 May 2022
Figure 1. Backscattered electron images showing ( a ) occurrence and mineral associations of chukochenite and ( b ) euhedral chukochenite crystals among fluorite crystals. Abbreviations: Ckc = chukochenite; Fl = fluorite; Na-M = Na-matgarite.