Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Mineralogical ClassificationIMA 2013-035 and 2013-036 = wulffite and parawulffite

26th Mar 2015 12:12 UTCMarco E. Ciriotti Manager

Reference:

▪ Pekov, I.V., Zubkova, N.V., Yapaskurt, V.O., Belakovskiy, D.I., Chukanov, N.V., Lykova, I.S., Savelyev, D.P., Sidorov, E.G., Pushcharovsky, D.Yu. (2014): Wulffite, K3NaCu4O2(SO4)4, and parawulffite, K5Na3Cu8O4(SO4)8, two new minerals from fumarole sublimates of the Tolbachik Volcano, Kamchatka, Russia. [i]Canadian Mineralogist[/i], [b]52[/b], 699-716.


Abstract:

Two chemically and structurally related new minerals were discovered in fumarolic sublimates at the Second scoria cone of the Northern Breakthrough of the Great Tolbachik Fissure Eruption, Tolbachik volcano, Kamchatka, Russia: wulffite, K3NaCu4O2(SO4)4, in the Arsenatnaya fumarole with euchlorine, aphthitalite, tenorite, hematite, lammerite, johillerite, fluoborite, etc., and parawulffite, K5Na3Cu8O4(SO4)8, in the Yadovitaya fumarole with euchlorine, fedotovite, hematite, langbeinite, steklite, etc. Later, parawulffite was found in sublimates of fumaroles related to the 2012–2013 Tolbachik Fissure Eruption. Both minerals form prismatic crystals (wulffite: up to 1.2 × 2 mm; parawulffite: up to 0.3 × 1 mm) in clusters and crusts. They are transparent with vitreous luster, brittle, with Mohs’ hardness ca 2½. Both minerals are dark green or deep emerald-green. D(meas.) is 3.23(2) and 3.35(2), and D(calc.) is 3.19 and 3.32 g cm–3 for wulffite and parawulffite, respectively. Both minerals are optically biaxial (+); wulffite: α 1.582(3), β 1.610(3), γ 1.715(3) and parawulffite: α 1.585(3), γ 1.717(4). Chemical data (wt.%, electron-microprobe; first value is for wulffite, second one for parawulffite) are: Na2O 4.11, 5.61; K2O 16.46, 13.74; Rb2O 0.95, 1.42; Cs2O 0.65, 1.21; CuO 38.88, 38.79; ZnO 0.15, 0.18; SO3 39.11, 39.26; total 100.31, 100.21. The empirical formulae are: wulffite (based on 18 O apfu): Na1.08(K2.85Rb0.08Cs0.04)Σ2.97(Cu3.99Zn0.02)Σ4.01S3.99O18; parawulffite (based on 36 O apfu): Na2.95(K4.75Rb0.25Cs0.14)Σ5.14(Cu7.95Zn0.04)Σ7.99S7.99O36. Wulffite is orthorhombic, [i]Pn[/i]21[i]a[/i], [i]a[/i] 14.2810(6), [i]b[/i] 4.9478(2), [i]c[/i] 24.1127(11) Å, [i]V[/i] 1703.79(13) Å3, [i]Z[/i] = 4. Parawulffite is monoclinic, [i]P[/i]2/[i]c[/i], [i]a[/i] 13.9043(10), [i]b[/i] 4.9765(3), [i]c[/i] 23.5855(17) Å, β 90.209(6)°,[i] V[/i] 1631.98(19) Å3, [i]Z[/i] = 2. The strongest reflections of their X-ray powder patterns [d,Å(I)(hkl)] are: wulffite: 9.27(100)(102), 7.16(22)(200), 3.125(16)(313, 215), 2.882(16)(411), 2.780(33)(117), 2.725(14)(413), 2.472(20)(020); parawulffite: 9.06(100)(-102, 102), 7.00(23)(200), 3.096(31)(313, -215), 2.736(33)(-117, 117), 2.492(24)(020), 2.321(26)(019, 513). The crystal structures of both minerals, solved from single-crystal X-ray diffraction data [[i]R[/i] = 0.0721 (wulffite) and 0.0985 (parawulffite)], are closely related with respect to parts of the heteropolyhedral quasi-framework formed by the Cu–O–S chains (built up of Cu2+-centered square pyramids and SO4 tetrahedra) and the chains of NaO6 octahedra. The new minerals differ from one another in ratios of alkali cations and their arrangement in cavities of the quasi-framework and in the configuration of Cu–O–S chains. Wulffite is named in honor of the Russian crystallographer Georgiy Viktorovich Wulff (1863–1925), who suggested the model of X-ray interference in crystals (1913). The name of parawulffite reflects its similarity to wulffite.

4th Apr 2015 18:16 UTCKnut Edvard Larsen 🌟 Manager

Mineral pages and locality pages updated.
 
Mineral and/or Locality  
Mindat Discussions Facebook Logo Instagram Logo Discord Logo
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: April 25, 2024 20:31:17
Go to top of page