1-20 OF 60 RESULTS FOR

obertiite

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 June 2017
Mineralogical Magazine (2017) 81 (3): 641–651.
...Roberta Oberti; Massimo Boiocchi; Frank C. Hawthorne; Neil A. Ball; Gȕnter Blass Abstract Pink-orange crystals of a composition within the ferri-obertiite compositional space were found in vesicles in a pale beige silicate vein found from a basalt quarry at Mount Rothenberg, Eifel district, Germany...
FIGURES
Journal Article
Published: 01 April 2010
The Canadian Mineralogist (2010) 48 (2): 301–306.
...Frank C. Hawthorne; Neil A. Ball; Gerald K. Czamanske Abstract Ferro-obertiite, Na Na 2 (Fe 2+3 Fe 3+ Ti) Si 8 O 22 O 2 , is a new mineral species of the amphibole group from Coyote Peak, Humboldt County, California, U.S.A., associated with inclusions of lithic-wacke sandstone in an alkali-rich...
FIGURES
Journal Article
Published: 01 December 2008
European Journal of Mineralogy (2008) 20 (6): 1011–1018.
... solution between potassic-obertiite and potassic-fluoro-magnesio-arfvedsonite. Zoning toward the rims increases the potassic-fluoro-magnesio-arfvedsonite component up to K Na 2 (Mg 3.5 Fe 3+ 1.5 ) Si 8 O 22 (F 1 (OH) 0.5 O 0.5 ). Table 1. Representative EMP analyses in wt. % oxides and unit formulae...
FIGURES | View All (4)
Journal Article
Published: 01 January 2000
American Mineralogist (2000) 85 (1): 236–241.
...Frank C. Hawthorne; Mark A. Cooper; Joel D. Grice; Luisa Ottolini Abstract Obertiite is a new amphibole species from Bellerberg, Laccher See district, Eifel, Germany. It occurs with tridymite, fluororichterite, hematite, rutile, aegirine-augite, kinoshitalite, and fluor-apatite in vugs in volcanic...
FIGURES
Image
Published: 01 April 2010
TABLE 5. COMPARISON OF SELECTED PHYSICAL PROPERTIES OF FERRO-OBERTIITE AND OBERTIITEX-R ay P owder -D iffraction P attern
Image
(a) The rock specimen containing holotype ferri-obertiite (scale in cm); (b) pink ferri-obertiite crystals with thin tabular sanidine crystals and alpha quartz paramorphic after beta quartz in an analogous rock specimen from the same quarry (courtesy of Marko Burkhardt; collection: Marko Burkhardt; field of view: 1.5  mm).
Published: 01 June 2017
Fig. 1. ( a ) The rock specimen containing holotype ferri-obertiite (scale in cm); ( b ) pink ferri-obertiite crystals with thin tabular sanidine crystals and alpha quartz paramorphic after beta quartz in an analogous rock specimen from the same quarry (courtesy of Marko Burkhardt; collection
Image
Published: 01 April 2010
TABLE 2. CHEMICAL COMPOSITION AND UNIT FORMULA OF FERRO-OBERTIITE*
Image
Published: 01 April 2010
TABLE 3. X-RAY POWDER-DIFFRACTION PATTERN OF FERRO-OBERTIITE
Image
Published: 01 April 2010
TABLE 4. SITE POPULATIONS FOR FERRO-OBERTIITE*C hemical C omposition
Image
Possible local configurations around the O3 sites in end-member obertiite; the O3 sites (unshaded circles) are always occupied by O2−.
Published: 01 January 2000
F igure 1. Possible local configurations around the O3 sites in end-member obertiite; the O3 sites (unshaded circles) are always occupied by O 2− .
Image
Possible local configurations around the O3 sites in obertiite; the O3 sites can be occupied by O2− or (OH,F). Possible amounts of local configurations compatible with the bulk composition of Table 1 are shown. The unshaded circles are O2−, the unshaded double circles are (OH,F).
Published: 01 January 2000
F igure 2. Possible local configurations around the O3 sites in obertiite; the O3 sites can be occupied by O 2− or (OH,F). Possible amounts of local configurations compatible with the bulk composition of Table 1 are shown. The unshaded circles are O 2− , the unshaded double circles are (OH,F).
Image
(a) A comparison of yangite (Downs et al. 2016) viewed down b with wollastonite-1A (Ohashi and Finger 1978) viewed down c. (b) A comparison of amphibole (obertiite, Hawthorne et al. 2000) with clinepyroxene (diopside, Thompson and Downs 2008), both viewed down c.
Published: 01 November 2016
Figure 12 ( a ) A comparison of yangite ( Downs et al. 2016 ) viewed down b with wollastonite-1 A ( Ohashi and Finger 1978 ) viewed down c . ( b ) A comparison of amphibole (obertiite, Hawthorne et al. 2000 ) with clinepyroxene (diopside, Thompson and Downs 2008 ), both viewed down c .
Journal Article
Published: 01 February 2018
American Mineralogist (2018) 103 (2): 330–337.
...Dmitriy I. Belakovskiy; Fernando Cámara; Yulia Uvarova; Olivier C. Gagné In this issue This New Mineral Names has entries for 15 new minerals, including abuite, achalaite, arrojadite-(BaNa), burroite, ferri-obertiite, hermannjahnite, jörgkellerite, leószilárdite, magnesiovesuvianite, mianningite...
Journal Article
Published: 01 December 2013
European Journal of Mineralogy (2013) 25 (6): 935–945.
...-magnesio-arfvedsonite, while composition A is a Fe 2+ , Fe 3+ and C Na rich variety of potassic-obertiite. Composition B is characterized by an exceptional high value of C □. It is emphasized that the presence of C □ and C Na in amphibole needs to be confirmed by other methods. The relationship between W O...
FIGURES | View All (5)
Journal Article
Published: 01 October 2004
Mineralogical Magazine (2004) 68 (5): 825–830.
..., which cannot be fitted into the four major amphibole groups. New root-names such as sodic-pedrizite in the Mg-Fe-Mn-Li group and obertiite and dellaventuraite in the sodic group along with two new prefixes, parvo and magno have also been added. As result it has become necessary to modify the AMPH-IMA97...
FIGURES
Journal Article
Published: 01 May 2004
American Mineralogist (2004) 89 (5-6): 883–887.
... is herein slightly, but significantly changed from the original idealized formula), necessitate amendments to the IMA 1997 definitions of the Mg-Fe-Mn-Li, calcic, sodic-calcic and sodic groups. The discovery of obertiite and the finding of an incompatibility in the IMA 1997 subdivision of the sodic group...
FIGURES
Journal Article
Published: 01 February 2004
Mineralogical Magazine (2004) 68 (1): 209–215.
..., but significantly, from the original idealized formula), necessitate amendments to the IMA 1997 definitions of the Mg-Fe-Mn-Li, calcic, sodic-calcic and sodic groups. The discovery of obertiite and the finding of an incompatibility in the IMA 1997 subdivision of the sodic group, requires further amendments within...
FIGURES
Journal Article
Published: 01 January 2004
European Journal of Mineralogy (2004) 16 (1): 191–196.
..., such as sodicpedrizite (which is herein slightly, but significantly changed from the original idealised formula), necessitate amendments to the IMA 1997 definitions of the Mg-Fe-Mn-Li, calcic, sodic-calcic and sodic groups. The discovery of obertiite and the finding of an incompatibility in the IMA 1997 subdivision...
FIGURES
Journal Article
Published: 01 December 2003
The Canadian Mineralogist (2003) 41 (6): 1355–1362.
... is herein slightly, but significantly, changed from the original idealized formula), necessitate amendments to the IMA 1997 definitions of the Mg–Fe–Mn–Li, calcic, sodic-calcic and sodic groups. The discovery of obertiite and the finding of an incompatibility in the IMA 1997 subdivision of the sodic group...
FIGURES
Journal Article
Published: 01 May 2011
American Mineralogist (2011) 96 (5-6): 936–945.
...(80,041,123,1̅33), 3.867(70,1̅31,121), and 3.664(70,030). F.C. Hawthorne, N.A. Ball, and G.K. Czamanske (2010) Ferro-obertiite, Na Na 2 (Fe 3 2+ Fe 3+ Ti) Si 8 O 22 O 2 , a new mineral species of the amphibole group from Coyote Peak, Humboldt county, California. Can. Mineral, 48, 301–306. Ferro...