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Mn2/Mn3

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The crystal structure of gatehouseite viewed in a direction close to [301İ]...
Published: 01 December 2011
F ig . 2. The crystal structure of gatehouseite viewed in a direction close to [301İ]. The Mn1ϕ 6 (ϕ: unspecified ligand) octahedra are red; Mn5ϕ 6 octahedra are orange; H atoms are shaded grey. The Mn2, Mn3 and Mn4 polyhedra have been omitted for clarity.
Image
Best-fit reconstruction of the Norwegian Sea prior to final opening of the ...
Published: 01 July 2009
Figure 1 Best-fit reconstruction of the Norwegian Sea prior to final opening of the northeast Atlantic (magnetic anomaly 24), adapted from Scott (2000) , showing locations of wells discussed in this paper and inferred source areas for sand types MN1, MN2, MN3, MN4, and MN5 (from Morton et al
Image
Early Neogene Rhinocerotidae taxa recorded from selected localities mention...
Published: 01 November 2021
) Moghara Jebel Zelten Rusinga Bézian and La Romieu Sansan Al-Sarrar Ad Dabtiyah Age (MN) MN3 MN2 MN3 MN3 MN3 MN4 MN6 MN5 MN5 Rhinocerotidae cf. Gaindatherium sp. (R), Brachypotherium cf. B . snowi (T) Gaindatherium cf. G . browni (R), cf. Rhinoceros (R
Image
Selected interatomic distances (in Å) in luboržákite.             Sb1–S1  2...
Published: 10 June 2020
2.6140(17) Mn2/Mn2’–S5 v 2.702(3) Mn2/Mn2’–S5 xii 2.702(3) As2/As2’–S2 2.657(2) As2/As2’–S3 2.4835(18) Mn3–S1 i 2.6209(17) As2/As2’–S3 ii 2.4835(18) Mn3–S1 2.6209(17) As2/As2’–S4 2.591(3) Mn3–S1 viii 2.6209(17) As2/As2’–S5 v 2.884(2) Mn3–S1 vii 2.6209(17
Journal Article
Published: 01 November 2008
American Mineralogist (2008) 93 (11-12): 1851–1857.
..., was refined using 1717 unique reflections to R = 4.1%. The site populations at the three independent octahedral sites, Mn1, Mn2, and Mn3, are Mn 0.82 Al 0.06 Mg 0.09 Cu 0.03 , Mn 0.75 Al 0.25 , and Mn 0.95 Al 0.05 , respectively. In agreement with a bond-valence analysis, three crystal-chemically different OH...
FIGURES | View All (5)
Journal Article
Published: 01 February 2021
American Mineralogist (2021) 106 (2): 174–179.
...) <Mn2-O> 2.217 Al-O9 1.829(4) P3-O11 1.542(3) Al-O5 1.845(4) P3-O12 1.543(4) Mn3-O12 2.117(4) Al-OH17 1.899(4) <P3-O> 1.534 Mn3-O3 2.160(3) Al-OW20 1.936(4) Mn3-O8 2.165(3) Al-OW19 1.940(4) P4-O13 1.542(4) Mn3-O15 2.189(4) Al-OH17 1.941(4) P4-O14...
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Mediterranean Province brachiopod genera of Floian and Dapingian (Arenig) a...
Published: 12 October 2021
Treiorworth Formation, Anglesey La Maurerie Formation Cluse de l’Orb Formation Foulon Formation Landeyran Formation B4 B3 W3 W4 W5 W6 E1 A3 A4 KA M Ar MN2 MN3 MN4 LINGULOIDEA Glossella + Ectenoglossa + + Elliptoglossa
Journal Article
Published: 01 December 2011
Mineralogical Magazine (2011) 75 (6): 2823–2832.
...F ig . 2. The crystal structure of gatehouseite viewed in a direction close to [301İ]. The Mn1ϕ 6 (ϕ: unspecified ligand) octahedra are red; Mn5ϕ 6 octahedra are orange; H atoms are shaded grey. The Mn2, Mn3 and Mn4 polyhedra have been omitted for clarity. ...
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(a)  Polyhedral sketch of the structure of Mn(OH) 2  and projection of the ...
Published: 01 February 2005
F igure 5. (a) Polyhedral sketch of the structure of Mn(OH) 2 and projection of the structure onto the a-b plane with representation of the Mn-Mn1, Mn-Mn2, and Mn-Mn3 pairs and illustration of the Mn-Mn1-Mn3 focusing effect. (b) Fourier transforms of the Mn-EXAFS spectra for the scale
Image
Polyhedral representation of the crystal structure of waterhouseite, ideall...
Published: 01 August 2005
- and Mn3-centered octahedra are striped. The unit cell is outlined. View approximately along [201], approximately perpendicular to the arsenoclasite-type strips of octahedra (Mn1- and Mn4-centered octahedra) and perpendicular to the finite chains of octahedra (Mn2- and Mn3-centered octahedra); note
Journal Article
Published: 01 June 2016
European Journal of Mineralogy (2016) 28 (3): 687–696.
... U 23 U 13 U 12 Mn1 0.9614(3) 0.58628(18) 0.26437(14) 0.0238(7) 0.0210(15) 0.0110(14) 0.0400(17) 0.0017(9) 0.0063(10) −0.0004(10) Mn2 0.5628(3) 0.58800(18) 0.26092(14) 0.0233(7) 0.0200(14) 0.0149(15) 0.0349(16) 0.0021(9) 0.0018(10) −0.0001(10) Mn3 0.4562(3...
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Journal Article
Published: 01 August 2014
American Mineralogist (2014) 99 (8-9): 1528–1536.
...) −0.00111(11) −0.00038(11) Mn2 1 0.080799(13) 0.085516(11) 0.50091(4) 0.00453(5) 0.00647(10) 0.00338(9) 0.00374(10) −0.00068(8) −0.00047(7) −0.00019(7) Mn3 1 0.084147(13) 0.330131(12) 0.24966(4) 0.00435(5) 0.00428(9) 0.00483(9) 0.00394(9) 0.00071(7) 0.00030(7) −0.00057(7) Mn4...
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Journal Article
Published: 01 July 2009
Journal of Sedimentary Research (2009) 79 (7): 540–553.
...Figure 1 Best-fit reconstruction of the Norwegian Sea prior to final opening of the northeast Atlantic (magnetic anomaly 24), adapted from Scott (2000) , showing locations of wells discussed in this paper and inferred source areas for sand types MN1, MN2, MN3, MN4, and MN5 (from Morton et al...
FIGURES | View All (11)
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The corner-sharing connections of the Mn 4 O 4  heterocubanes in a structur...
Published: 01 August 2014
Figure 5 The corner-sharing connections of the Mn 4 O 4 heterocubanes in a structural moiety cutting out parallel to (110) of the low-temperature form of the LiMn 2 O 4 spinel. The lithium atoms are eliminated for clarity. The four types of Mn 4 O 4 heterocubanes, i.e., Mn2 4 O9 4 , Mn3 2 Mn4
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Early Miocene paleogeographic map (modified from Popov et al.,  2004 ) show...
Published: 01 November 2021
Figure 6. Early Miocene paleogeographic map (modified from Popov et al., 2004 ) showing selected localities mentioned in the text. ( 1 ) The Negev, early Miocene, MN3, Israel; ( 2 ) Bugti Hills (Upper Member of Chitarwata Formation), early Miocene, MN2, Pakistan; ( 3 ) Moghara, early Miocene
Journal Article
Published: 01 April 2017
Mineralogical Magazine (2017) 81 (2): 319–327.
.... The only direct linkages between heteropolyhedral layers are via hydrogen bonds. Table 6. Bond-valence sums for mesaite. Ca Mn1 Mn2 Mn3 V1 V2 V3 H-bonds Σ a O1 0.42 1.43 +0.11,+0.07 2.03 O O2 0.33 0.39 1.37 2.09 O O3 0.37 0.33 1.34...
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Sites, site occupancy factors, atom factional coordinates, and equivalent i...
Published: 10 June 2020
) *Mn2/Mn2’ ½ 0 0 0.0384(7) *As3/As3’ 0.23266(10) 0 0.11593(9) 0.0383(5) Mn3 ½ ½ ½ 0.0202(6) S1 0.64205(17) 1 0.52920(13) 0.0159(6) S2 0.56273(17) ½ 0.35382(13) 0.0200(7) S3 0.34236(19) 0 0.24368(15) 0.0251(8) S4 0.3725(2) ½ 0.05194(16) 0.0344(9) S5
Journal Article
Published: 01 August 2005
The Canadian Mineralogist (2005) 43 (4): 1401–1410.
...- and Mn3-centered octahedra are striped. The unit cell is outlined. View approximately along [201], approximately perpendicular to the arsenoclasite-type strips of octahedra (Mn1- and Mn4-centered octahedra) and perpendicular to the finite chains of octahedra (Mn2- and Mn3-centered octahedra); note...
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Journal Article
Published: 01 April 2008
American Mineralogist (2008) 93 (4): 573–583.
... distances are also much smaller than the other octahedral distances in melanotekite. In kentrolite, distances Mn1-O9, Mn2-O1, Mn3-O9, and Mn3-O1 behave in the same way. T able 13. Pb 2 Fe 2 Si 2 O 9 —Selected interatomic distances (Å) and bond angles (°) M1 Angle (°) M2...
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Journal Article
Published: 10 June 2020
Mineralogical Magazine (2020) 84 (5): 738–745.
... 2.6140(17) Mn2/Mn2’–S5 v 2.702(3) Mn2/Mn2’–S5 xii 2.702(3) As2/As2’–S2 2.657(2) As2/As2’–S3 2.4835(18) Mn3–S1 i 2.6209(17) As2/As2’–S3 ii 2.4835(18) Mn3–S1 2.6209(17) As2/As2’–S4 2.591(3) Mn3–S1 viii 2.6209(17) As2/As2’–S5 v 2.884(2) Mn3–S1 vii 2.6209(17...
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