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Hetaerolite

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Journal Article
Published: 01 December 1973
American Mineralogist (1973) 58 (11-12): 1065–1068.
...George Udubasa; Joachim Ottemann; George Agiorgitis Abstract A new occurrence of hetaerolite from Rodna/Rumania is described and detailed mineralogical and chemical investigations undertaken. 6 3 1973 21 6 1973 Copyright © 1973 by the Mineralogical Society of America 1973...
Journal Article
Published: 01 January 1942
American Mineralogist (1942) 27 (1): 48–56.
...Clifford Frondel; E. WM. Heinrich Abstract Hetaerolite, ZnMn 2 O 4 , is isostructural with hausmannite, MnMn 2 O 4 . Weissenberg x -ray study of type hetaerolite gave: a 0 = 5.74, c 0 = 9.15; a 0 : c 0 = 1:1.594, a : c = 1.5952 (morph.); cell contents Zn 4 Mn 8 O 16 . The hetaerolite described...
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Reflectance spectra of Pb and Zn ‘oxide’ minerals: 1, <span class="search-highlight">hetaerolite</span>;2, hydroh...
Published: 01 May 2007
Fig. 3 Reflectance spectra of Pb and Zn ‘oxide’ minerals: 1, hetaerolite;2, hydrohetaerolite; 3, franklinite;4, coronadite; 5, zincite; 6, minium;7, plattnerite; 8, bindheimite;9, wulfenite; 10, vanadinite;11, descloizite; 12, gahnite.
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Reflectance spectra of Pb and Zn ‘oxide’ minerals: 1, <span class="search-highlight">hetaerolite</span>;2, hydroh...
Published: 01 May 2007
Fig. 3 Reflectance spectra of Pb and Zn ‘oxide’ minerals: 1, hetaerolite;2, hydrohetaerolite; 3, franklinite;4, coronadite; 5, zincite; 6, minium;7, plattnerite; 8, bindheimite;9, wulfenite; 10, vanadinite;11, descloizite; 12, gahnite.
Journal Article
Published: 01 October 2014
American Mineralogist (2014) 99 (10): 1956–1961.
..., corresponding to the dehydration of chalcophanite followed by transformation to a spinel structure (Mn-hetaerolite). Only small changes were observed in the chalcophanite unit cell from RT to ~438 K; the volume increased by ~0.8%, mostly caused by thermal expansion of ~0.5% along c . Above ~427 K...
FIGURES | View All (5)
Journal Article
Published: 01 August 2002
American Mineralogist (2002) 87 (8-9): 1121–1127.
... with the highest hetaerolite content. T-O bond distance (2.027–2.041 Å) shows a strong positive correlation with unit-cell constants, while the O-T-O angle (103.3–103.7°) is related only to the oxygen coordinate, z . The two octahedral bond distances show limited variations: the shorter one, M-O S , ranges from...
FIGURES | View All (4)
Journal Article
Published: 01 October 1965
American Mineralogist (1965) 50 (10): 1670–1680.
...Clifford Frondel; Cornelis Klein, Jr. Abstract Metallographic, x -ray diffraction and electron micro-probe observations have been made on exsolution growths of hetaerolite, gahnite and hematite in analyzed specimens of franklinite from franklin and Sterling Hill, New Jersey. The hetaerolite...
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EDS analyses of FE-SEM ( Figure 10 ): (a) beudantite; (b) baryte; (c) smith...
Published: 01 April 2018
Figure 11. EDS analyses of FE-SEM ( Figure 10 ): (a) beudantite; (b) baryte; (c) smithsonite; (d) hetaerolite; (e) illite; (f) Mn oxide.
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FE-SEM images of different minerals in the sulfides weathered to limonite o...
Published: 01 April 2018
Figure 10. FE-SEM images of different minerals in the sulfides weathered to limonite or the siderite weathered to limonite: (a) beudantite; (b) baryte; (c) smithsonite; (d) hetaerolite; (e) illite; (f) Mn oxide.
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Polyhedral structure drawings for: ( a ) anhydrous chalcophanite and ( b ) ...
Published: 01 October 2014
Figure 5 Polyhedral structure drawings for: ( a ) anhydrous chalcophanite and ( b ) Mn-rich hetaerolite projected down c . Mn-O octahedra are colored pink, and Zn-O polyhedra are yellow. The O atoms are indicated by red and blue [O(3)] spheres. (Color online.)
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Structure drawings of: ( a ) chalcophanite, ( b ) anhydrous chalcophanite, ...
Published: 01 October 2014
Figure 1 Structure drawings of: ( a ) chalcophanite, ( b ) anhydrous chalcophanite, and ( c ) Mn-rich hetaerolite. Mn-O octahedra are colored pink, and Zn-O polyhedra are yellow. The O atoms are indicated by red and blue [O(3)] spheres. For all three structures the c axis is vertical. (Color
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Final observed (red crosses), calculated (green solid line), and difference...
Published: 01 October 2014
Figure 2 Final observed (red crosses), calculated (green solid line), and difference (purple below) powder X-ray diffraction patterns from the Rietveld refinement for: ( a ) chalcophanite, ( b ) anhydrous chalcophanite, and ( c ) Mn-rich hetaerolite. The Bragg reflections are marked by the set
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False color fieldscan images of selected samples, analyzed by QEMSCAN. Less...
Published: 01 June 2015
Fig. 5 False color fieldscan images of selected samples, analyzed by QEMSCAN. Less abundant and trace minerals are not visible in the figure, and are therefore not represented in the color key. The latter phases comprise Fe dolomite, pyrite, hetaerolite, Fe-Mn (hydr)oxides, chalcophanite
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False color fieldscan images of selected samples and their concentrates, an...
Published: 01 June 2015
Fig. 6 False color fieldscan images of selected samples and their concentrates, analyzed by QEMSCAN. Less abundant and trace minerals are not visible in the figure and are not represented in the color key. Theses phases comprise Fe dolomite, pyrite, hetaerolite, Fe-Mn (hydr)oxides, chalcophanite
Journal Article
Published: 01 August 1987
American Mineralogist (1987) 72 (7-8): 812–815.
... is associated with hetaerolite, clinohedrite, hodgkinsonite, and willemite from Franklin, Sussex County, New Jersey. Crystal-structure analysis shows it to be a zincosilicate isotypic with minerals of the chlorite group. Copyright © 1987 by the Mineralogical Society of America 1987 ...
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False color fieldscan images of two thin sections analyzed by QEMSCAN: J109...
Published: 01 June 2015
Fig. 4 False color fieldscan images of two thin sections analyzed by QEMSCAN: J109-5 from a core sample and Js-Mon 2 from a surface specimen. Less abundant and trace minerals are not represented in the color key. The latter phases comprise Fe dolomite, pyrite, hetaerolite, Fe-Mn (hydr)oxides
Journal Article
Journal: Economic Geology
Published: 01 January 1961
Economic Geology (1961) 56 (1): 198–203.
...B. L. Sreenivas; Rustum Roy Abstract The behavior of cations in some manganese minerals was studied by electrodialysis. Among the common manganese oxide minerals, psilomelane, hollandite, lithiophorite, chalcophanite and hetaerolite showed no change. Cryptomelane (alpha -MnO 2 ) shows significant...
Journal Article
Journal: Economic Geology
Published: 01 January 1960
Economic Geology (1960) 55 (1): 1–55.
... to be persistently supergene: groutite, hydrohausmannite, lithiophorite, rancieite, hetaerolite, hydrohetaerolite, chalcophanite, crednerite, woodruffite, and wad. Another group of oxides appears to have been formed only by hypogene processes: manganosite, hausmannite, pyrochroite, bixbyite, galaxite, jacobsite...
Journal Article
Published: 01 April 1956
American Mineralogist (1956) 41 (3-4): 268–275.
... of the constituent elements occurs on heating, and the recombination of these oxides to form hetaerolite, ZnMn 2 O 4 , at higher temperatures indicates hydrohetaerolite is a separate mineral species distinct from the former. A method of density determination for fibrous minerals is described. Copyright © 1956...
Journal Article
Published: 01 April 1955
American Mineralogist (1955) 40 (3-4): 349–353.
... powder pattern. From the cell dimensions, the structures of Mn 3 0 4 and ZnMn 2 0 4 (hetaerolite) are evidently similar, and a further close analogy may well exist between Frondel's new mineral and hydrohetaerolite which also contains “structural water” (Frondel and Heinrich 1942). The writer recently...