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sursassite

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Journal Article
Published: 01 September 2022
American Mineralogist (2022) 107 (9): 1760–1765.
..., of a single crystal of Mg-sursassite, Mg 5 Al 5 Si 6 O 21 (OH) 7 . In situ high-pressure and high-temperature single-crystal diffraction allowed the study of structural variation at non-ambient conditions and the determination of bulk elastic properties. The refined parameters of a second-order Birch...
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Journal Article
Published: 01 September 2020
American Mineralogist (2020) 105 (9): 1432–1435.
...Luca Bindi; Mark D. Welch; Aleksandra A. Bendeliani; Andrey V. Bobrov Abstract The crystal structure of a new high-pressure hydrous phase, Si-rich Mg-sursassite, of ideal composition Mg 4 Al 5 Si 7 O 23 (OH) 5 , that was produced by sub-solidus reaction at 24 GPa and 1400 °C in an experiment using...
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Journal Article
Published: 01 October 2009
American Mineralogist (2009) 94 (10): 1440–1449.
...Mariko Nagashima; Masahide Akasaka; Tetsuo Minakawa; Eugen Libowitzky; Thomas Armbruster Abstract The crystal chemistry of sursassite, simplified formula Mn 2 2+ Al 3 Si 3 O 11 (OH) 3 , from six different localities [(1) Falotta, Switzerland, (2) Woodstock, New Brunswick, Canada, (3) Kamisugai...
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Journal Article
Published: 01 November 2008
American Mineralogist (2008) 93 (11-12): 1851–1857.
.... The weight loss from TG measurement is 7.7 wt% at 1000 °C, most of which is interpreted to be due to the loss of structural OH groups. The crystal structure of macfallite [ a = 8.959(3), b = 6.072(2), c = 10.218(4) Å, β = 110.75(3)°, space group P 2 1 / m ], which is isostructural with sursassite...
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First thumbnail for: Crystal chemistry of macfallite: Relationships to ...
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Journal Article
Published: 01 October 2008
European Journal of Mineralogy (2008) 20 (5): 993–998.
...Frédéric Hatert; Andre-Mathieu Fransolet; Johan Wouters; Heinz-Jürgen Bernhardt Abstract Sursassite occurs as orange-red needles associated with nsutite, hematite, apatite-(CaF), spessartine, manganoan clinochlore, and ardennite in quartz veinlets cross-cutting the red-purple schists...
FIGURES
First thumbnail for: The crystal structure of <span class="search-highl...
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Journal Article
Published: 01 May 2002
European Journal of Mineralogy (2002) 14 (3): 575–580.
...Bernd WUNDER; Matthias GOTTSCHALK Abstract Sursassites (Fe,Mg) 4 (Mg,Al,Fe) 2 Al 4 [Si 6 O 21 / (OH) 7 ] have been synthesized along the Mg-Fe join at 4.0 - 5.0 GPa, 600 - 650 °C and at f 02 defined by the iron-wuestite buffer using gels as starting materials. (Fe,Mg)-sursassites have been...
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Journal Article
Published: 01 September 2000
European Journal of Mineralogy (2000) 12 (5): 935–945.
... been determined by the Rietveld method, and found to be isostructural with sursassite rather than pumpellyite. This phase is therefore a slightly modified Mg-analogue of sursassite Mn 2+ 4 Al 2 Al 4 [Si 6 O 22 /(OH) 6 ], with Mg for Mn and one Al replaced by Mg+H. For material synthesized at 5 GPa...
FIGURES
First thumbnail for: Crystal structure of the high-pressure phase Mg 4 ...
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Journal Article
Published: 01 February 1964
American Mineralogist (1964) 49 (1-2): 168–173.
...R. L. Freed Abstract The geology and mineralogy of sursassite from New Brunswick have been described by Heinrich (1962). Sursassite from the only other known locality, Oberhalbstein, Graubünden, Switzerland, has been analyzed chemically by Müller (1916), Jakob (1926, 1931, 1933), and de Quervain...
Journal Article
Published: 01 December 1962
The Canadian Mineralogist (1962) 7 (2): 291–300.
...E. William Heinrich Abstract Sursassite, previously known only from Oberhalbstein, Graubunden, Switzerland, occurs in veinlets cutting Middle Silurian Fe-Mn ores about 5 mi W. of Woodstock, New Brunswick. The composition based on a new analysis is Mn 9 Al 4 (Si,Al) 12 O 39 .6H 2 O. Associated...
Image
a) Zero-loss energy filtered HRTEM image of Mg-sursassite perpendicular to [001], showing no stacking faults; b) HRTEM image of Mg-sursassite showing domains; c) HRTEM image of Mg-sursassite perpendicular to [001] showing twin boundaries along a (010) glide plane with a translation of a/2.
Published: 01 September 2000
Fig. 6. a) Zero-loss energy filtered HRTEM image of Mg-sursassite perpendicular to [001], showing no stacking faults; b) HRTEM image of Mg-sursassite showing domains; c) HRTEM image of Mg-sursassite perpendicular to [001] showing twin boundaries along a (010) glide plane with a translation
Image
X-ray powder diffraction pattern of run product P97 (98 wt% Mg-sursassite, 2 wt% enstatite) in the 2𝛉 range 30–39°. For comparison the calculated and indexed X-ray pattern of Mg-sursassite (solid line) and of MgMgAl-pumpellyite (dashed line) are shown. Abbreviations: e = enstatite, s = Mg-sursassite, p = MgMgAl-pumpellyite. For further explanations see text.
Published: 01 September 2000
Fig. 5. X-ray powder diffraction pattern of run product P97 (98 wt% Mg-sursassite, 2 wt% enstatite) in the 2𝛉 range 30–39°. For comparison the calculated and indexed X-ray pattern of Mg-sursassite (solid line) and of MgMgAl-pumpellyite (dashed line) are shown. Abbreviations: e = enstatite, s
Journal Article
Published: 01 December 1999
American Mineralogist (1999) 84 (11-12): 1906–1914.
... be described as layers of X-octahedra shifted by (1/2,0,0) vectors. The shifted layers locally show a sursassite-type arrangement. No disorder was detected in the Y-octahedra, which are fully occupied by Al ions, and in the W positions, commonly hosting sevenfold-coordinated Ca atoms in naturally occurring...
Image
Evolution of the density of Mg-sursassite along a P-T path representative of the top (solid line) and bottom (dashed line) of a cold subducting slab (based on the isoviscous model of van Keken et al. 2002). Thermodynamic data for forsterite (Fo) are from Holland and Powell (2011). Mg-sursassite is indicated as Mg-surs. Density has been calculated using the equation of state for solids from Holland and Powell (2011). (Color online.)
Published: 01 September 2022
Figure 5. Evolution of the density of Mg-sursassite along a P-T path representative of the top (solid line) and bottom (dashed line) of a cold subducting slab (based on the isoviscous model of van Keken et al. 2002 ). Thermodynamic data for forsterite (Fo) are from Holland and Powell (2011
Image
Variations of unit-cell parameters (Å) as a function of CaMn1+(Mg+Cu+Mn+Fe)M1+M3 (apfu); e.s.d. values of plotted values are considerably smaller than the symbol size. Closed circles denote sursassites in this study. Open diamond denotes sursassite data obtained by Hatert et al. (2008). Sample numbers are given in Tables 1 and 2.
Published: 01 October 2009
F igure 3. Variations of unit-cell parameters (Å) as a function of Ca Mn1 +(Mg+Cu+Mn+Fe) M1+M3 (apfu); e.s.d. values of plotted values are considerably smaller than the symbol size. Closed circles denote sursassites in this study. Open diamond denotes sursassite data obtained by Hatert et al
Image
P-T-diagram showing the stability-field of Mg-sursassite as determined by Fockenberg (1998). The linear 6 °C/km geotherm was calculated for a mean rock density of 3.3 g/cm3. P-T-paths for cold and warm subduction zones are taken from Thompson (1992). Squares indicate P-T-conditions and numbers give the wt.% of FeO for sursassite synthesized by Domanik &amp; Holloway (1996).
Published: 01 May 2002
Fig. 1. P-T-diagram showing the stability-field of Mg-sursassite as determined by Fockenberg (1998) . The linear 6 °C/km geotherm was calculated for a mean rock density of 3.3 g/cm 3 . P-T-paths for cold and warm subduction zones are taken from Thompson (1992) . Squares indicate P-T-conditions
Journal Article
Published: 01 October 2008
European Journal of Mineralogy (2008) 20 (5): 735–744.
..., and at higher pressures up to 4 GPa pyrope forms from chlorite + talc + kyanite. Beyond 4 GPa, the assemblage talc + chlorite + Mg-chloritoid defines the lower temperature limit around 600 °C. At pressures higher than 5 GPa, pyrope forms via the reactions low-clinoenstatite + chlorite + Mg-sursassite = pyrope...
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Evolution of the unit-cell volume of Mg-sursassite with pressure. The solid line represents the second-order BM-EoS fit.
Published: 01 September 2022
Figure 2. Evolution of the unit-cell volume of Mg-sursassite with pressure. The solid line represents the second-order BM-EoS fit.
Image
Evolution of the unit-cell volume of natural sursassite with pressure. The solid line represents the second-order BM-EoS fit.
Published: 01 September 2022
Figure 3. Evolution of the unit-cell volume of natural sursassite with pressure. The solid line represents the second-order BM-EoS fit.
Image
Evolution of the unit-cell volume of Mg-sursassite with temperature. Data were fitted with a Berman type EoS (solid line).
Published: 01 September 2022
Figure 4. Evolution of the unit-cell volume of Mg-sursassite with temperature. Data were fitted with a Berman type EoS (solid line).
Image
ATR-FTIR spectrum of sursassite between 3800–2400 cm−1.
Published: 01 October 2009
F igure 1. ATR-FTIR spectrum of sursassite between 3800–2400 cm −1 .