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mukhinite

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Journal Article
Published: 01 June 2010
The Canadian Mineralogist (2010) 48 (3): 523–536.
... to anhedral dissakisite-(La), mukhinite, and clinozoisite are associated with V- and Cr-rich garnet (goldmanite – grossular – uvarovite solid-solution), V- and Cr-rich muscovite, amphibole-group minerals (magnesiohornblende, tremolite, actinolite, and edenite), diopside, titanite, albite, quartz, siderite...
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Journal Article
Published: 21 May 2018
Mineralogical Magazine (2018) 82 (4): 889–911.
... . Epidote-supergroup minerals occur as abundant anhedral crystals with variable compositional zoning. Nearly all crystals have a complete zoning sequence beginning with REE -rich allanite-(La), followed by mukhinite and by V- and Cr-rich clinozoisite to mukhinite and V- and Cr-poor clinozoisite. In common...
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Journal Article
Published: 01 January 2008
American Mineralogist (2008) 93 (1): 63–73.
...–36 mol% uvarovite, and 9–59 mol% grossular end-members). The garnet is unzoned or shows V-rich cores and Al-rich rims, or irregular coarse oscillatory zoning with V, Cr, and Al, locally involving Ca and Mn as well. The V,Cr-rich clinozoisite to mukhinite and “chromian clinozoisite” contains 2–9.5 wt...
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Image
Nomenclature of monoclinic ternary Al-Fe-Cr epidote minerals. Analogue diag...
Published: 02 January 2004
Figure 1. Nomenclature of monoclinic ternary Al-Fe-Cr epidote minerals. Analogue diagrams for other solid solutions (e.g., with V = mukhinite as an endmember) can be used.
Image
Back-scattered electron images of epidote-supergroup and associated mineral...
Published: 21 May 2018
Fig. 5. Back-scattered electron images of epidote-supergroup and associated minerals: ( a ) Isolated grain of epidote-supergroup mineral with distinct clinozoisite-mukhinite (Czo-Muk) and clinozoisite (Czo) zones overgrown by chlorite (Chl) and pyrite (Py); ( b ) Czo-Muk in association
Image
Back-scattered electron images of garnets and associated minerals: ( a ) pr...
Published: 21 May 2018
with clinozoisite-mukhinite (Czo-Muk), sphalerite (Sph) and pyrite (Py).
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BSE images of EGM in the samples studied. A) Zoned crystal of EGM with rim ...
Published: 01 June 2010
, amphibole and quartz (sample RY–10). C) Crystal of EGM with markedly developed dissakisite-(La) zone (sample KRY–5A). Symbols: Ab: albite, Am: amphibole, Czo: clinozoisite, Dis: dissakisite-(La), Muk: mukhinite, Qtz: quartz, Py: pyrite, Sd: siderite, Ttn: titanite.
Published: 01 January 2013
EISBN: 9780903056434
.... Piemontites are strongly coloured and pleochroic in yellows, pinks and reds (Fig. 46 ); the low-manganese variety withamite is much paler in colour and is only weakly pleochroic. Piemontite is distinguished from other epidote group minerals, except mukhinite (cations Ca 2 Al 2 V 3+ ) and members...
FIGURES
Published: 01 January 2013
EISBN: 9780903056434
... epidotes, however, do contain appreciable amounts and show transitional characters towards allanite. Rare chromian (tawmawite), plumbian (hancockite) and vanadium-bearing (mukhinite) epidotes have been described. At temperatures above ~730°C there is continuous solid solution between clinozoisite...
FIGURES
Journal Article
Published: 01 April 2008
European Journal of Mineralogy (2008) 20 (2): 261–269.
... for crystal-structure refinement . University of Göttingen , Germany . Shepel , A.V. & Karpenko , M.V. ( 1969 ): Mukhinite, a new vanadium species of epidote . Doklady of the Academy of Sciences of the U.S.S.R., Earth Science Sections , 185 , 123 – 126 . Sokolova , E.V...
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Journal Article
Published: 01 August 2013
Mineralogical Magazine (2013) 77 (6): 2739–2752.
...+ -rich epidote-supergroup minerals is uncommon. The V 3+ -analogue of clinozoisite, mukhinite, simplified formula Ca 2 Al 2 V 3+ (SiO 4 )(Si 2 O 7 )O(OH), and the V 3+ -analogue of androsite, vanadoandrosite-(Ce), Mn 2+ Ce 3+ V 3+ AlMn 2+ (SiO 4 )(Si 2 O 7 )O(OH), are known ( Shepel and Karpenko, 1969...
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Journal Article
Published: 01 September 2006
European Journal of Mineralogy (2006) 18 (5): 551–567.
... have to be described as chromian (or better Cr 3+ -rich) clinozoisite until new evidence is presented. Mukhinite , Ca 2 Al 2 V 3+ [Si 2 O 7 ][SiO 4 ]O(OH), was described by Shepel & Karpenko (1969) from marbles (Gornaya Shoriya, Kemerovo Oblast, Siberia, Russia). The name...
FIGURES
Journal Article
Published: 01 October 2009
European Journal of Mineralogy (2009) 21 (5): 1073–1080.
.... Epidote supergroup 3 3 Reference: Armbruster et al . (2006) . Epidote group Allanite group Dollaseite group Clinozoisite Allanite-(Ce) Dollaseite-(Ce) Epidote Allanite-(La) Khristovite-(Ce) Epidote-(Pb) Allanite-(Y) Mukhinite Dissakisite-(Ce) Clinozoisite-(Sr...
Journal Article
Published: 01 February 2011
The Canadian Mineralogist (2011) 49 (1): 195–206.
.../10. References Bacik P. Uher P. ( 2010 ): dissakisite-(La), mukhinite, and clinozoisite: (V,Cr,REE)-rich members of the epidote group in amphibole – pyrite – pyrrhotite metabasic rocks from Pezinok, Rybníček mine, Western Carpathians, Slovakia . Can. Mineral. 48 , 523 – 536...
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Journal Article
Published: 01 September 2006
European Journal of Mineralogy (2006) 18 (5): 569–582.
... pattern can be extended to the REE-free mukhinite ( Shepel & Karpenko, 1969 ), for which one rather expects Al in M1 (and M2) and V 3+ in M3 on the basis of ionic size, but this awaits structural confirmation. As to the V-rich (up to ca. 9 wt% V 2 O 3 ), Mn-poor ‘allanites’ analysed by Pan &...
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Journal Article
Published: 01 October 2002
The Canadian Mineralogist (2002) 40 (5): 1411–1419.
... cerian mukhinite “ REE -enriched epidote”. The formula for allanite-(Ce) is commonly given as (Ce,Ca,Y) 2 (Al,Fe 2+ ,Fe 3+ ) 3 (SiO 4 ) 3 (OH) ( e.g. , Mandarino 1999 ). However, note that: There are two large cation sites, one that strongly prefers Ca, the other, Ln ; thus the formula...
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Journal Article
Journal: Economic Geology
Published: 01 June 2020
Economic Geology (2020) 115 (4): 771–791.
...), with concentrations mostly exceeding 100 ppm ( Fig. 11 ). Substitution of Mn, Sr, and V represent the solid-solution series toward piemontite, epidote-Sr, and mukhinite, respectively. Titanium and Mg were also frequently detected by microprobe (also see Cooke et al., 2014b ; Baker et al., 2020 ), which, with its...
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Journal Article
Published: 01 October 2011
European Journal of Mineralogy (2011) 23 (5): 731–743.
... 3 O 12 (OH) (“tawmawite”) and Ca 2 Al 2 V 3+ Si 3 O 12 (OH) (mukhinite). The individual site-specific cation concentrations for crystals 1A and 1C slightly deviate ( e.g ., Ca deficiency) from ideal values ( Table 2 ). This is probably due to low crystallinity of this sample as discussed below...
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Journal Article
Published: 01 February 2002
Mineralogical Magazine (2002) 66 (1): 137–150.
... Al O Epidote Ca Ca Al Al Fe 3+ O Mukhinite Ca Ca Al Al V 3+ O Hancockite Ca Pb Al Al Fe 3+ O Piemontite Ca Ca Al Al Mn 3+ O Strontiopiemontite Ca Sr Al Al Mn 3+ O Tweddillite Ca Sr Mn 3+ Al Mn 3+ O REE -bearing minerals of the epidote...
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Series: Special Publications of the Society of Economic Geologists, Special Publications of the Society of Economic Geologists
Published: 01 January 2014
DOI: 10.5382/SP.18.07
EISBN: 9781629499291
... Epidote Ca 2 Al 2 Fe 3+ [Si 2 O 7 ][SiO 4 ]O(OH) Epidote-(Sr) CaSrAl 2 Fe 3+ [Si 2 O 7 ][SiO 4 ]O(OH) Epidote-(Pb) CaPbAl 2 Fe 3+ [Si 2 O 7 ][SiO 4 ]O(OH) Clinozoisite Ca 2 Al 3 [Si 2 O 7 ][SiO 4 ]O(OH) Clinozoisite-(Sr) CaSrAl 3 [Si 2 O 7 ][SiO 4 ]O(OH) Mukhinite Ca 2 Al 2 V 3+ [Si 2...
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