Alacranite, AS8S9:: structural study of the holotype and re-assignment of the original chemical formula

被引:27
作者
Bonazzi, P
Bindi, L
Popova, V
Pratesi, G
Menchetti, S
机构
[1] Univ Florence, Dipartimento Sci Terra, I-50121 Florence, Italy
[2] Univ Florence, Museo Storia Nat, Sez Mineral & Litol, Florence, Italy
[3] RAS, Urals Branch, Inst Mineral, Miass 456317, Russia
关键词
D O I
10.2138/am-2003-11-1220
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Alacranite from the type locality (Uzon caldera, Kamchatka, Russian Federation) was submitted for structural analysis. A single crystal was selected and the following lattice parameters were determined: a = 9.942(4), b = 9.601(2), c = 9.178(3) Angstrom, beta = 101.94(3)degrees, V = 857.1 (5) Angstrom(3). The crystal structure was solved in the P2/c space group using direct methods and refined to R = 6.79% for 472 observed reflections. The structure of alacranite consists of an ordered sequence of As4S4 and As4S5 cage-like molecules, with a molecular packing closely resembling that found in the beta-As4S4 phase. Both As-As and As-S intramolecular distances are in the range usually observed for covalent bonds. The structural model confirms the chemical formula As8S9 for alacranite, and accounts for differences in the unit-cell parameters of alacranite compared to those of the natural analogue of beta-As4S4. This latter mineral, therefore, should receive a new name.
引用
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页码:1796 / 1800
页数:5
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