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![(a) Mid-infrared thermal emissivity spectra of sulfates with chains of SO4 tetrahedra and MX6 octahedra, including amarantite, zincobotryogen, butlerite, parabutlerite, copiapite/ferricopiapite, magnesiocopiapite, and sideronatrite. In addition, the crystal structure diagrams are shown [amarantite from Süsse (1968); botryogen from Süsse (1967); butlerite from Fanfani et al. (1971); ferricopiapite from Fanfani et al. (1973); and metasideronatrite from Ventruti et al. (2010)]. Band depths have been adjusted by multiplying the spectra by the parenthetical amounts; spectra are then offset for clarity. (b–e) VNIR reflectance spectra of sulfates with chains of SO4 tetrahedra and MX6 octahedra including: (b) amarantite, botryogen, butlerite, and parabutlerite; (c) copiapite from 0.4–5 μm, Mg-copiapite, and sideronatrite from 0.4–5 μm; (d) three grain size fractions of amarantite from 0.3–2.65 μm; and (e) three particle-size fractions of botryogen from 0.3–2.65 μm.]()
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![(a) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between ~0.80 and 1.12 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: butlerite (Fanfani et al. 1971), parabutlerite (Borene 1970a), slavikite (Parafiniuk et al. 2010), fibroferrite (Scordari 1981), botryogen (Süsse 1967), and zincobotryogen (Süsse 1968a). O atoms are shown in red, OH in gray, H in pink, Mg in yellow, and Fe in orange. (Color online.) (b) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between 0.94 and 1.22 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: sideronatrite and metasideronatrite [Ventruti et al. (2010); metasideronatrite has the same structural unit topology as sideronatrite; Scordari and Ventruti (2009)], metahohmannite (Scordari et al. 2004), amarantite (Süsse 1968b), jarosite (Basciano and Peterson 2007), and plumbojarosite (Szymanski 1988). Note the presence of a magnetic phase impurity in plumbojarosite. O atoms are shown in red, H in pink, Mg in yellow, and Fe in orange. (c) Mössbauer spectra and Fe coordination polyhedra in sulfates without nominal Fe in their structures. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: anhydrite (Hawthorne and Ferguson 1975) and celestine (Miyake et al. 1978). O atoms are shown in red, Ca in blue, and Sr in green. Neither of these minerals is likely to contain much Fe because of the large size of the coordination polyhedra as seen here; these are configured to accommodate the Ca2+ cation, which is significantly larger than Fe3+. Thus although the hand sample of SPT132 is mostly anhydrite, XRD reveals a significant component of coquimbite, which dominates the spectrum of the mixture because it is so much more Fe rich. Celestine ML-S13 is pure by XRD, but some Fe-rich phase is present there, too, at low concentrations. These data cannot discriminate between Fe in the celestine structure and Fe in an impurity. (Color online.)]()
![(a) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between ~0.80 and 1.12 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: butlerite (Fanfani et al. 1971), parabutlerite (Borene 1970a), slavikite (Parafiniuk et al. 2010), fibroferrite (Scordari 1981), botryogen (Süsse 1967), and zincobotryogen (Süsse 1968a). O atoms are shown in red, OH in gray, H in pink, Mg in yellow, and Fe in orange. (Color online.) (b) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between 0.94 and 1.22 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: sideronatrite and metasideronatrite [Ventruti et al. (2010); metasideronatrite has the same structural unit topology as sideronatrite; Scordari and Ventruti (2009)], metahohmannite (Scordari et al. 2004), amarantite (Süsse 1968b), jarosite (Basciano and Peterson 2007), and plumbojarosite (Szymanski 1988). Note the presence of a magnetic phase impurity in plumbojarosite. O atoms are shown in red, H in pink, Mg in yellow, and Fe in orange. (c) Mössbauer spectra and Fe coordination polyhedra in sulfates without nominal Fe in their structures. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: anhydrite (Hawthorne and Ferguson 1975) and celestine (Miyake et al. 1978). O atoms are shown in red, Ca in blue, and Sr in green. Neither of these minerals is likely to contain much Fe because of the large size of the coordination polyhedra as seen here; these are configured to accommodate the Ca2+ cation, which is significantly larger than Fe3+. Thus although the hand sample of SPT132 is mostly anhydrite, XRD reveals a significant component of coquimbite, which dominates the spectrum of the mixture because it is so much more Fe rich. Celestine ML-S13 is pure by XRD, but some Fe-rich phase is present there, too, at low concentrations. These data cannot discriminate between Fe in the celestine structure and Fe in an impurity. (Color online.)]()
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1-13 OF 13 RESULTS FOR
zincobotryogen
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Journal Article
New Mineral Names, Free
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 February 2018
American Mineralogist (2018) 103 (2): 330–337.
..., pharmazincite, riotintoite, wiklundite, żabińskiite, and zincobotryogen. M.A. Galliski, M.F. Márquez-Zavalía, P. Černý, R. Lira, F. Colombo, A.C. Roberts, and H.-J. Bernhardt (2016) Achalaite, Fe 2+ TiNb 2 O 8 , a new member of the wodginite group from the La Calandria granitic pegmatite, Córdoba...
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![(a) Mid-infrared thermal emissivity spectra of sulfates with chains of SO4 tetrahedra and MX6 octahedra, including amarantite, zincobotryogen, butlerite, parabutlerite, copiapite/ferricopiapite, magnesiocopiapite, and sideronatrite. In addition, the crystal structure diagrams are shown [amarantite from Süsse (1968); botryogen from Süsse (1967); butlerite from Fanfani et al. (1971); ferricopiapite from Fanfani et al. (1973); and metasideronatrite from Ventruti et al. (2010)]. Band depths have been adjusted by multiplying the spectra by the parenthetical amounts; spectra are then offset for clarity. (b–e) VNIR reflectance spectra of sulfates with chains of SO4 tetrahedra and MX6 octahedra including: (b) amarantite, botryogen, butlerite, and parabutlerite; (c) copiapite from 0.4–5 μm, Mg-copiapite, and sideronatrite from 0.4–5 μm; (d) three grain size fractions of amarantite from 0.3–2.65 μm; and (e) three particle-size fractions of botryogen from 0.3–2.65 μm.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/ammin/100/1/10.2138_am-2015-4762/3/s_0066f3.jpeg?Expires=2147483647&Signature=vo66UXwOITYUA773DMZ1W7HoaNCqOh5Wo4Pi5EEIuJRAVEYgoE2tvNOwUbveaVxZ~VhPmQ15IFVg3A9xUQywq18bOWQt7QfuGg8oWMjN5OkykrfZdvqJQejr-jCuK~W1up6YLFAuyp854P2a0iuQ4lGkEgQKTMwPVbFPolZWjyKRokcVhPokQJjtKMCznrRmOf1Kp5hzHBxAq8VLGYobGcUpEEeGdqio1H1kAnGjT2qoFRrMwljdAkqKoBKkoxuadegkX-LNsA2lEoKJ5erzaeVCkw-B-8XseZLOsDGHzd-FIRT9k8pHct3jG6qYI5Oy13ZmmazRbklhZ9AQA6EFvQ__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
( a ) Mid-infrared thermal emissivity spectra of sulfates with chains of SO... Available to Purchase
in Mid-infrared emission spectroscopy and visible/near-infrared reflectance spectroscopy of Fe-sulfate minerals
> American Mineralogist
Published: 01 January 2015
Figure 3 ( a ) Mid-infrared thermal emissivity spectra of sulfates with chains of SO 4 tetrahedra and MX 6 octahedra, including amarantite, zincobotryogen, butlerite, parabutlerite, copiapite/ferricopiapite, magnesiocopiapite, and sideronatrite. In addition, the crystal structure diagrams
Journal Article
Mid-infrared emission spectroscopy of sulfate and sulfate-bearing minerals Available to Purchase
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 January 2007
American Mineralogist (2007) 92 (1): 1–18.
..., kainite, kieserite, linarite, minamiite, natrojarosite, pickeringite, plumbojarosite, polyhalite, potassium alum (potash alum; kalinite), rozenite, serpierite, sulfohalite, szomolnokite, thaumasite, thenardite, and zincobotryogen. T able 1. Listing of the sulfate-bearing minerals...
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Journal Article
New minerals and nomenclature modifications approved in 2016 Available to Purchase
Journal: Mineralogical Magazine
Published: 01 April 2016
Mineralogical Magazine (2016) 80 (2): 407–413.
... No. 30, April 2016, page 409; Mineralogical Magazine , 80 , 407–413. IMA No. 2015-107 Zincobotryogen ZnFe 3+ (SO 4 ) 2 (OH)·7H 2 O Xietieshan lead-zinc deposit, Qinghai Province, China Zhuming Yang*, Gerald Giester, Qian Mao, Yuguang Ma, Di Zhang and He Li *E-mail: yangzhm...
Journal Article
Mineralogy of the Paso Robles soils on Mars Available to Purchase
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 May 2008
American Mineralogist (2008) 93 (5-6): 728–739.
... 95830 Yavapaiite KFeSO 4 ML-S79 §§§ ML-S79§§§ ML-S79 §§§ Zincobotryogen (Zn,Mg,Mn)Fe(SO 4 ) 2 (OH)·7H 2 O C5525-3 C5525-3 The PR Phase 2 spectrum is also unusual for geologic materials associated with Mars to date and exhibits a reflectance maximum in the 904 and 934 nm...
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![(a) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between ~0.80 and 1.12 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: butlerite (Fanfani et al. 1971), parabutlerite (Borene 1970a), slavikite (Parafiniuk et al. 2010), fibroferrite (Scordari 1981), botryogen (Süsse 1967), and zincobotryogen (Süsse 1968a). O atoms are shown in red, OH in gray, H in pink, Mg in yellow, and Fe in orange. (Color online.) (b) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between 0.94 and 1.22 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: sideronatrite and metasideronatrite [Ventruti et al. (2010); metasideronatrite has the same structural unit topology as sideronatrite; Scordari and Ventruti (2009)], metahohmannite (Scordari et al. 2004), amarantite (Süsse 1968b), jarosite (Basciano and Peterson 2007), and plumbojarosite (Szymanski 1988). Note the presence of a magnetic phase impurity in plumbojarosite. O atoms are shown in red, H in pink, Mg in yellow, and Fe in orange. (c) Mössbauer spectra and Fe coordination polyhedra in sulfates without nominal Fe in their structures. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: anhydrite (Hawthorne and Ferguson 1975) and celestine (Miyake et al. 1978). O atoms are shown in red, Ca in blue, and Sr in green. Neither of these minerals is likely to contain much Fe because of the large size of the coordination polyhedra as seen here; these are configured to accommodate the Ca2+ cation, which is significantly larger than Fe3+. Thus although the hand sample of SPT132 is mostly anhydrite, XRD reveals a significant component of coquimbite, which dominates the spectrum of the mixture because it is so much more Fe rich. Celestine ML-S13 is pure by XRD, but some Fe-rich phase is present there, too, at low concentrations. These data cannot discriminate between Fe in the celestine structure and Fe in an impurity. (Color online.)](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/ammin/98/11-12/10.2138_am.2013.4604/3/s_1943f5a.jpeg?Expires=2147483647&Signature=T1tiiimHZXEnN0jzlK1USmqBnQMaBl7iJdC~A9Kxut37h7FRfZCAs6koU9OFJ3AamhiA38RzgbANylp2wzHCzDYZF7sUFzCmuar3wEu9q~pMY0UZfh9VHF7ViKQEEs9WntXKr1rLFqKN9frUIxzoWzoIex5oJ2hdMWV-H8h3pyr6Q4K1qG4ROINI9vCJDeHURDv5Uvd8tSblkjdS0gbOacrW61D7AeiUnla0VAnYj9ASiHCHKByd2WheeCrfYzBqzoEnOgRZxvexCvH4nM2IUl5YZGAMzrlvzOMN1jVb1RjdYXepaPf~yAGwqMZEqR~LFZZT7NJRTbuZzeufmQPMFw__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
( a ) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ va... Available to Purchase
Published: 01 November 2013
1970a ), slavikite ( Parafiniuk et al. 2010 ), fibroferrite ( Scordari 1981 ), botryogen ( Süsse 1967 ), and zincobotryogen ( Süsse 1968a ). O atoms are shown in red, OH in gray, H in pink, Mg in yellow, and Fe in orange. (Color online.) ( b ) Mössbauer spectra and Fe coordination polyhedra in sulfates
Image
![(a) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between ~0.80 and 1.12 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: butlerite (Fanfani et al. 1971), parabutlerite (Borene 1970a), slavikite (Parafiniuk et al. 2010), fibroferrite (Scordari 1981), botryogen (Süsse 1967), and zincobotryogen (Süsse 1968a). O atoms are shown in red, OH in gray, H in pink, Mg in yellow, and Fe in orange. (Color online.) (b) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ values between 0.94 and 1.22 mm/s. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: sideronatrite and metasideronatrite [Ventruti et al. (2010); metasideronatrite has the same structural unit topology as sideronatrite; Scordari and Ventruti (2009)], metahohmannite (Scordari et al. 2004), amarantite (Süsse 1968b), jarosite (Basciano and Peterson 2007), and plumbojarosite (Szymanski 1988). Note the presence of a magnetic phase impurity in plumbojarosite. O atoms are shown in red, H in pink, Mg in yellow, and Fe in orange. (c) Mössbauer spectra and Fe coordination polyhedra in sulfates without nominal Fe in their structures. Polyhedra were created using CrystalMaker software and data from the American Mineralogist Crystal Structure Database: anhydrite (Hawthorne and Ferguson 1975) and celestine (Miyake et al. 1978). O atoms are shown in red, Ca in blue, and Sr in green. Neither of these minerals is likely to contain much Fe because of the large size of the coordination polyhedra as seen here; these are configured to accommodate the Ca2+ cation, which is significantly larger than Fe3+. Thus although the hand sample of SPT132 is mostly anhydrite, XRD reveals a significant component of coquimbite, which dominates the spectrum of the mixture because it is so much more Fe rich. Celestine ML-S13 is pure by XRD, but some Fe-rich phase is present there, too, at low concentrations. These data cannot discriminate between Fe in the celestine structure and Fe in an impurity. (Color online.)](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/ammin/98/11-12/10.2138_am.2013.4604/3/s_1943f5b.jpeg?Expires=2147483647&Signature=C3FSnGbf8VxHJPE51qtEy6ZuYjTOQHT9a8quErSHPBrvAJRr0zWfnPsBq3P5JvgNYCKwvlnycZu6ebA3ufatoq0-htguPKQr3JHea5nj679WSDMeMCZl92ybEEAD1WRLWeSIC4DST-rXLVU4zmf5tm0b~9kfLbBDTm1NZq8vr0eiDNpKIu5dE2diGPL~jrFkPD8ETPZ1ue1x0cntU0614tEqKI0uFPLf-jOHKF7fRVY6~M~40E0085X17snOlGmwv7wrD6XJjgwWul0L4uvMMg3-jJxivpP9eLDZfWIu-Fov8i3hDyqwJU3Tqtu46I4fRxmwdxwSglx34OWiIZDVqw__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
( a ) Mössbauer spectra and Fe coordination polyhedra in sulfates with Δ va... Available to Purchase
Published: 01 November 2013
1970a ), slavikite ( Parafiniuk et al. 2010 ), fibroferrite ( Scordari 1981 ), botryogen ( Süsse 1967 ), and zincobotryogen ( Süsse 1968a ). O atoms are shown in red, OH in gray, H in pink, Mg in yellow, and Fe in orange. (Color online.) ( b ) Mössbauer spectra and Fe coordination polyhedra in sulfates
Journal Article
Crystal structure of sideronatrite-2 M , Na 2 Fe(SO 4 ) 2 (OH)(H 2 O) 3 , a new polytype from Xitieshan lead-zinc deposit, Qinghai Province, China Available to Purchase
Journal: European Journal of Mineralogy
Publisher: GeoScienceWorld Journals
Published: 01 June 2015
European Journal of Mineralogy (2015) 27 (3): 427–432.
... for the refinement of crystal structures . University of Göttingen , Germany . Tu , G. , Li , X. , Xie , X. , Yin , S. ( 1964 ): Zincobotryogen and zincocopiapite - Two new varieties of sulphate minerals . Sci. Geol. Sinica , 5 , 313 – 30 . (in Chinese). Ventruti , G. , Stasi...
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Includes: Supplemental Content
Journal Article
THE GLADSTONE–DALE COMPATIBILITY OF MINERALS AND ITS USE IN SELECTING MINERAL SPECIES FOR FURTHER STUDY Available to Purchase
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
Published: 01 October 2007
The Canadian Mineralogist (2007) 45 (5): 1307–1324.
..., tschermigite, ungemachite, vanthoffite, vlodavetsite, voltaite, vonbezingite, wherryite, woodwardite, wroewolfeite, xitieshanite, ye’elimite, zincobotryogen and zincovoltaite. Amarantite, letovicite, mountkeithite, potassium alum, glaucocerinite, leightonite, löweite, zircosulfate, rabejacite...
Journal Article
SULFATE MINERALS. I. BOND TOPOLOGY AND CHEMICAL COMPOSITION Available to Purchase
Journal: The Canadian Mineralogist
Publisher: Mineralogical Association of Canada
Published: 01 December 2006
The Canadian Mineralogist (2006) 44 (6): 1403–1429.
... with an average bond-valence of 0.20 vu ( Fig. 3b ). An O atom commonly links three ( M 3+ ϕ 6 ) octahedra and receives two additional bonds from the interstitial complex. Zincobotryogen, Zn(H 2 O) 5 Fe 3+ (OH) (H 2 O) 1 (SO 4 ) 2 (H 2 O), has the structural unit [Fe 3+ (SO 4 ) 2 (OH)(H 2 O) 1 ] 2...
FIGURES
Journal Article
Mid-infrared emission spectroscopy and visible/near-infrared reflectance spectroscopy of Fe-sulfate minerals Available to Purchase
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 January 2015
American Mineralogist (2015) 100 (1): 66–82.
...Figure 3 ( a ) Mid-infrared thermal emissivity spectra of sulfates with chains of SO 4 tetrahedra and MX 6 octahedra, including amarantite, zincobotryogen, butlerite, parabutlerite, copiapite/ferricopiapite, magnesiocopiapite, and sideronatrite. In addition, the crystal structure diagrams...
FIGURES
Includes: Supplemental Content
Journal Article
Mössbauer parameters of iron in sulfate minerals Available to Purchase
Journal: American Mineralogist
Publisher: Mineralogical Society of America
Published: 01 November 2013
American Mineralogist (2013) 98 (11-12): 1943–1965.
... 1970a ), slavikite ( Parafiniuk et al. 2010 ), fibroferrite ( Scordari 1981 ), botryogen ( Süsse 1967 ), and zincobotryogen ( Süsse 1968a ). O atoms are shown in red, OH in gray, H in pink, Mg in yellow, and Fe in orange. (Color online.) ( b ) Mössbauer spectra and Fe coordination polyhedra in sulfates...
FIGURES
Journal Article
The Crystal Chemistry of Sulfate Minerals Available to Purchase
Publisher: Mineralogical Society of America
Published: 01 January 2000
Reviews in Mineralogy and Geochemistry (2000) 40 (1): 1–112.
... 20h 22c,d [9] zincobotryogen [ZnFe 3+ (OH)(H 2 O) 6 (SO 4 ) 2 ](H 2 O) 10.517 17.847 7.133 – 100.1 – P 2 1 / n 20h 22c,d [10] kröhnkite Na 2 [Cu 2+ (H 2 O) 2 (SO 4 ) 2 ] 5.807 12.656 5.517 – 108.3 – P 2 1 / c 20e 22e,f [11] krausite K[Fe 3+ (H 2 O) 2 (SO 4 ) 2...
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