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pyroxenoid

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Journal Article
Published: 22 April 2019
Mineralogical Magazine (2019) 83 (3): 473–478.
.... Nagashima M. , Imaoka T. , Fukuda C. and Pettke T. ( 2018 ) Relationship between cation substitution and hydrogen-bond system in hydrous pyroxenoids with three-periodic single-chains of SiO 4 tetrahedra: pectolite, murakamiite, marshallsussmanite, serandite and tanohataite . European...
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Journal Article
Published: 01 February 2017
Mineralogical Magazine (2017) 81 (1): 183–197.
... with layers containing the NaO 4 (OH)(H 2 O) 2 polyhedra. The I -beam topology and the T–O–T stacking pattern present in nolzeite is similar to that found in other chain silicate minerals, specifically steedeite, as well as pyroxenoids of the pectolite (NaCa 2 [Si 3 O 8 OH])–sérandite (NaMn 2 [Si 3...
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Journal Article
Published: 01 June 2015
Mineralogical Magazine (2015) 79 (3): 671–686.
...R. H. Mitchell; M. D. Welch; A. R. Kampf; A. K. Chakhmouradian; J. Spratt Abstract The new pyroxenoid barrydawsonite-(Y) occurs at the Merlot Claim, North Red Wine Pluton, Labrador, Canada (62°32′38.54″ W; 54°08′1.37″ N). The host rock is a metamorphosed eudialyte syenite consisting of eudialyte...
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Journal Article
Journal: Economic Geology
Published: 01 December 1998
Economic Geology (1998) 93 (8): 1390–1405.
..., manganiferous, pyroxene-pyroxenoid, Ca-rich garnet alteration assemblages. The latter include hedenbergite, pyroxferroite-pyroxmangite, fayalite, calcic almandine, quartz, and apatite. Immobile element concentrations and mass balance considerations demonstrate that rocks with the pyroxene-pyroxenoid-garnet...
Journal Article
Published: 01 April 1992
American Mineralogist (1992) 77 (3-4): 380–390.
...Kenneth J. T. Livi; David R. Veblen Abstract Two occurrences of johannsenite partially altered to pyroxenoid minerals were studied by X-ray emission analytical electron microscopy in the context of the pyroxene-wollas-tonite polysomatic series in order to determine the relationships between...
Journal Article
Published: 01 June 1991
American Mineralogist (1991) 76 (5-6): 900–903.
...Ross J. Angel; Charles W. Burnham Abstract Previous discussions of the pyroxenoid and clinopyroxene crystal structures have noted the polysomatic relationship between them, in which pyroxenoids with chain periodicities greater than three contain both pyroxeno-like (P) and wollastonite-like (W...
Journal Article
Published: 01 April 1990
American Mineralogist (1990) 75 (3-4): 409–414.
...Donald R. Peacor; Pete J. Dunn; John S. White; Joel D. Grice; Peter H. Chi Abstract Lithiomarsturite, ideally LiCa 2 Mn 2 HSi 5 O 15 , is a new member of the p-p (pectolite-pyroxene) series of pyroxenoids (hydropyroxenoids). It has a structure based on fünferket-ten , but chain-periodicity faults...
Journal Article
Published: 01 October 1985
American Mineralogist (1985) 70 (9-10): 885–901.
...David R. Veblen Abstract A specimen of the CaMn clinopyroxene johannsenite that has partially reacted to Mn pyroxenoids has been studied with high-resolution transmission electron microscopy (HRTEM), electron diffraction, and single-crystal X-ray methods. The primary johannsenite is structurally...
Journal Article
Published: 01 February 1981
American Mineralogist (1981) 66 (1-2): 154–168.
Journal Article
Published: 01 October 1980
American Mineralogist (1980) 65 (9-10): 981–985.
...Friedrich Liebau Abstract In pyroxenoids containing cationic hydrogen [pectolite, schizolite, serandite, unnamed Ca(Sc,Fe 3+ )H[Si 3 O 9 ], synthetic Cd 2 NaH[Si 3 O 9 ], nambulite, Li-hydrorhodonite, santaclaraite, and babingtonite] the identity periods of the silicate chains are approximately...
Journal Article
Published: 01 April 1978
American Mineralogist (1978) 63 (3-4): 274–288.
Journal Article
Published: 01 December 1964
American Mineralogist (1964) 49 (11-12): 1527–1542.
...C. T. Prewitt; Donald R. Peacor Abstract The classification of the crystal structures of the pyroxenes and pyroxenoids according to the repeat unit of the silicate chain is well-known. This system does not, however, differentiate between structures which contain similar types of chains. For example...
Journal Article
Published: 01 June 1971
American Mineralogist (1971) 56 (5-6): 877–887.
Journal Article
Published: 01 November 2016
American Mineralogist (2016) 101 (11): 2544–2553.
...Richard M. Thompson; Hexiong Yang; Robert T. Downs Abstract A hypothetical ideal wollastonite with regular octahedra and T3 tetrahedron is presented and used to compare and contrast the pyroxenes and pyroxenoids. While clinopyroxenes have close-packed arrangements of oxygen anions, several lines...
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Journal Article
Published: 01 August 1996
American Mineralogist (1996) 81 (7-8): 822–832.
...D. Andrault; J. P. Itie; F. Farges Abstract The CaGeO 3 and SrGeO 3 perovskites and CaGeO 3 , SrGeO 3 , and MnGe0 3 pyroxenoids have been studied at high-temperature by X-ray diffraction (XRD) and X-ray absorption fine-structure spectroscopy (XAFS). The diffraction studies show that the back...
Journal Article
Published: 01 June 2010
European Journal of Mineralogy (2010) 22 (3): 393–402.
... is partially occupied. Five crystallographically independent octahedral sites are occupied by Mn (mainly Mn 2+ with 10–20 % Mn 3+ ), with additional small amounts of Ca and V 3+ . An undulating pyroxenoid-like chain is built by five SiO 4 tetrahedra. A sixth tetrahedron, forming a branch of the chain...
FIGURES
Journal Article
Published: 01 April 1981
American Mineralogist (1981) 66 (3-4): 278–289.
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<span class="search-highlight">PYROXENOID</span> MINERALS ISOSTRUCTURAL WITH SERANDITE–SCHIZOLITE–PECTOLITE
Published: 02 August 2021
TABLE 1. PYROXENOID MINERALS ISOSTRUCTURAL WITH SERANDITE–SCHIZOLITE–PECTOLITE
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Mn–Ca-(Fe + Mg) plot of <span class="search-highlight">pyroxenoid</span> compositions from the Luziyuan mine. Das...
Published: 18 January 2018
Figure 11. Mn–Ca-(Fe + Mg) plot of pyroxenoid compositions from the Luziyuan mine. Dashed lines indicate miscibility gap between rhodonite and bustamite at T = 550 °C (Abrecht & Peters, 1980 ).
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The relationships between the pyroxene and <span class="search-highlight">pyroxenoid</span> O-chains for ( a ) rh...
Published: 01 November 2016
Figure 10 The relationships between the pyroxene and pyroxenoid O-chains for ( a ) rhodonite ( Peacor et al. 1978 ), ( b ) pyroxmangite ( Zanazzi et al. 2008 ), and ( c ) ferrosilite III ( Weber 1983 ), which have T-chain repeat lengths of 5, 7, and 9, respectively.