- ►arizona.edu [PDF] AR Kampf - Canadian Mineralogist, 2005 - canmin.geoscienceworld.org The crystal structure of cobaltarthurite, ideally Co 2+ Fe 3+ 2 (AsO 4 ) 2 (OH)
2 ·4H 2 O, monoclinic, P2 1 /c, a 10.2635(9), b 9.7028(8), c 5.5711(5) Å, ß
94.2070(10)°, from Khder, Bou Azzer district, Morocco, has been refined to ... Related articles - BL Direct - All 6 versions
[CITATION] Die Kristallstruktur von Arthurit, CuFe3+ 2 [(H2O)|(OH) 2|(AsO4) 2]
- ►arizona.edu [PDF] JL Jambor, J Vinals, LA Groat, M Raudsepp - Canadian Mineralogist, 2002 - canmin.geoscienceworld.org Cobaltarthurite, of ideal end-member formula Co 2+ Fe 3+ 2 (AsO 4 ) 2 (OH) 2
·4H 2 O, is a new Co-dominant member of the arthurite group and is named to
reflect that relationship. The new species occurs predominantly as ... Cited by 2 - Related articles - BL Direct - All 4 versions
- ►arizona.edu [PDF] M Raudsepp, E Pani - Canadian Mineralogist, 2002 - canmin.geoscienceworld.org The crystal structure of cobaltarthurite from near Pastrana, southeastern Spain
[monoclinic, a 10.2694(4), b 9.6790(3), c 5.5723(2) Å, ß 94.277(2)°, P2 1
/c], has been refined to R wp and R B indices of 7.7 and 1.7%, ... Cited by 2 - Related articles - BL Direct - All 5 versions
DY Pushcharovskii, M Pasero, S Merlino, NV … - Crystallography Reports, 2002 - Springer The zirconosilicate seidozerite was discovered by EI Semenov in 1958 in the
Lovozero alkaline massif [1]. This mineral belongs to a rather large group of
(Zr,Ti)-silicates, whose structures contain three-layer heteropolyhedral ... Cited by 5 - Related articles - BL Direct - All 4 versions
JM Hughes, ES Bloodaxe, KD Kobel, JW … - MINERALOGICAL MAGAZINE, 1996 - rruff.geo.arizona.edu OJUELAITEwas described from its occurrence at the Ojuela mine in Mapimi, Mexico
by Cesbron et al. (1981). Those authors suggested that the phase was
isostructural with whitmoreite (Moore et at., 1974), a phase of interest ... Related articles - View as HTML
- ►arizona.edu [PDF] DY Pushcharovsky, YS Lebedeva, NV Zubkova … - Canadian Mineralogist, 2004 - canmin.geoscienceworld.org Sturmanite, ideally Ca 6 Fe 2 3+ (SO 4 ) 2.5 [B(OH) 4 ](OH) 12 ·25H 2 O, is
trigonal, P31c, Z = 2, with a 11.188(9), c 21.91(7) Å, V 2375.1(5) Å 3 . The
crystal structure has been refined to an R index of 0.079. As in the case ... Cited by 3 - Related articles - BL Direct - All 5 versions
