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Leucophoenicite

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Journal Article
Published: 01 August 1986
American Mineralogist (1986) 71 (7-8): 985–988.
...Yu-Chyi Yau; Donald R. Peacor Abstract tem images of jerrygibbsite from Franklin, New Jersey, reveal random and ordered mixed layering with leucophoenicite on (001) and periodic twinning that gives rise to complex superperiodicites within the leucophoenicite. The differences between the structures...
Journal Article
Published: 01 January 2002
American Mineralogist (2002) 87 (1): 154–159.
...Mark D. Welch; William G. Marshall; Nancy L. Ross; Kevin S. Knight Abstract The proton positions in leucophoenicite, ideally Mn 7 Si 3 O 12 (OH) 2 , have been determined by neutron powder diffraction under ambient conditions on a natural sample from Franklin, New Jersey. Refinement in the P 2 1...
FIGURES
Journal Article
Published: 01 August 1995
American Mineralogist (1995) 80 (7-8): 676–679.
... alternating with thinner goethite-like (G) slabs in the ordered arrangements O ∞ , OOOG, and OG. Leucophoenicite, OOOG, containing the same kind of slabs, represents the only macroscopic member of the leucophoenicite series (White and Hyde, 1983). It has the same slab sequence as the hydrous B phase; lamellar...
Journal Article
Published: 01 February 1993
American Mineralogist (1993) 78 (1-2): 190–194.
...) for all reflections. Ribbeite is structurally related to leucophoenicite in that it contains serrated, edge-sharing chains of Mn octahedra and two distinct types of Si tetrahedral sites: (1) a single, isolated, fully occupied Si tetrahedron, and (2) a pair ofedge-sharing, half-occupied Si tetrahedra...
Journal Article
Published: 01 October 1988
American Mineralogist (1988) 73 (9-10): 1182–1185.
... mcgovemite in the absence of Zn, and the substitution of Al for most of the Fe 3+ . Analytical data for two new occurrences of leucophoenicite, from the Kombat mine and from the Italian Alps, show that this mineral is Ca-bearing, does not contain essential Zn, and has not yet been found as the ideal end...
Journal Article
Published: 01 February 1987
American Mineralogist (1987) 72 (1-2): 213–216.
... of the leucophoenicite group having octahedron sequence (1,2 2 ) 2 and is the unit-cell-twinned equivalent of alleghanyite. It occurs in Mn-rich silicate-carbonate units within lenses of manganese oxide ores as equigranular grains associated with alleghanyite, manganoan calcite, pyrochroite, chlorite, galaxite...
Journal Article
Published: 01 June 1984
American Mineralogist (1984) 69 (5-6): 546–552.
...Pete J. Dunn; Donald R. Peacor; William B. Simmons; Eric J. Essene Abstract Jerrygibbsite, ideally Mn 9 (SiO 4 ) 4 (OH) 2 , is polymorphous with the Mn-humite sonolite, and a probable member of the leucophoenicite group. It occurs as intergrown grains with a typical metamorphic texture at Franklin...
Journal Article
Published: 01 October 1983
American Mineralogist (1983) 68 (9-10): 1009–1021.
...Timothy J. White; Bruce G. Hyde Abstract Three leucophoenicite specimens were examined in the transmission electron microscope and by X-ray powder diffraction and electron-probe microanalysis. A comparison of observed and computer-simulated structure images supports Moore’s proposals...
Journal Article
Published: 01 August 1970
American Mineralogist (1970) 55 (7-8): 1146–1166.
...Paul B. Moore Abstract Leucophoenicite, a 10.842 (19), b 4.826 (6), c 11.324 (9) Å, β 103.93° (9), P2 1 /a, possesses the crystallochemical formula Mn 7 [SiO 4 ] 2 [(SiO 4 )(OH) 2 ], with two formula units in the crystal cell. The atomic arrangement was deciphered from Patterson synthesis; atomic...
Journal Article
Published: 01 October 1969
American Mineralogist (1969) 54 (9-10): 1392–1398.
... to be a valid species, identical with the materia] of Palache (1910), but the later studies of this mineral by Palache (1928, 1935) and Moore (1967) are composite descriptions of leucophoenicite, sonolite and alleghanyite. Some still undescribed chemical variants of minerals in the chondrodite and olivine...
Journal Article
Published: 01 August 1967
American Mineralogist (1967) 52 (7-8): 1226–1232.
...Paul B. Moore Abstract Leucophoenicite, 3Mn 2 SiO 4 ·Mn(OH) 2 , is generally regarded as a member of the manganese humite group. However, unlike the monoclinic members alleghanyite, 2Mn 2 SiO 4 ·Mn(OH) 2 , and sonolite, 4Mn 2 SiO 4 ·Mn(OH) 2 , which seem to be normal members of the manganese humite...
Image
Neutron powder diffraction patterns of <span class="search-highlight">leucophoenicite</span> for PEARL&#x2F;HiPr (top)...
Published: 01 January 2002
F igure 2. Neutron powder diffraction patterns of leucophoenicite for PEARL/HiPr (top) and POLARIS (bottom) data sets for the 90° detector banks. In both patterns data are shown as crosses and the calculated pattern is shown as a continuous line and the difference (observed-calculated) pattern
Image
The environment of protons in <span class="search-highlight">leucophoenicite</span> determined by neutron powder ...
Published: 01 January 2002
F igure 3. The environment of protons in leucophoenicite determined by neutron powder diffraction. ( a ) The P 2 1 / a structure in which two half-occupied Si1 tetrahedra share a common edge (O7-O7). The inversion center lies midway along the O7-O7 edge and is indicated by a double circle
Journal Article
Published: 01 April 1985
American Mineralogist (1985) 70 (3-4): 379–387.
...Pete J. Dunn Abstract The manganese humites, (alleghanyite, manganhumite, and sonolite), together with some Mn-bearing samples of the Mg-humites, and the related phases leucophoenicite and jerrygibbsite, from the orebodies at Franklin and Sterling Hill, New Jersey, are described together...
Image
Photomicrograph showing an imperfect octahedron of brownish yellow oxyplumb...
Published: 01 October 2013
F ig . 1. Photomicrograph showing an imperfect octahedron of brownish yellow oxyplumboroméite on a matrix of calcite (white) and leucophoenicite (pink).
Image
(a)  Polyhedral sketch of a portion of the structure common to mineral spec...
Published: 01 February 2005
F igure 6. (a) Polyhedral sketch of a portion of the structure common to mineral species from the olivine-, humite-, and leucophoenicite-group of minerals. SiO 4 tetrahedra (dark gray) are linked by edges and corners to MnO 6 octahedra (light gray). After Fujino et al. (1981) . (b
Journal Article
Published: 01 October 2013
Mineralogical Magazine (2013) 77 (7): 2931–2939.
...F ig . 1. Photomicrograph showing an imperfect octahedron of brownish yellow oxyplumboroméite on a matrix of calcite (white) and leucophoenicite (pink). ...
FIGURES | View All (5)
Journal Article
Published: 01 May 2000
American Mineralogist (2000) 85 (5-6): 792–800.
.... The arrangement of cation octahedra within a single chain has the same basic structural unit of five edge-sharing octahedra found in olivine, the humite group, and leucophoenicite. Carmichaelite is inferred to have co-precipitated with its pyrope host and other titanates in the presence of a fluid or melt phase...
FIGURES | View All (4)
Journal Article
Published: 01 December 1989
American Mineralogist (1989) 74 (11-12): 1355–1359.
...Joel D. Grice; Pete J. Dunn Abstract Sclarite, ideally (Zn,Mg,Mn) 4 Zn 3 (CO 3 ) 2 (OH) 10 , is a new mineral species from the Franklin mine, New Jersey. It occurs as 1.5-mm clusters of clear, colorless crystals associated with leucophoenicite, gageite, zincite, and willemite. The mineral has...
Journal Article
Published: 01 June 1988
American Mineralogist (1988) 73 (5-6): 632–636.
...); moderate dispersion, r < v ; X = b, Z ∧ c = 45(3)°. Holdawayite forms coarse veins cutting silicate-facies Mn-bearing rocks with assemblages including humite- and/or leucophoenicite-group minerals. Idealized Cl-free holdawayite, Mn 3 (CO 3 )(OH) 4 , may form by hydration of rhodochrosite and in turn may...