University of Adelaide Library

Adelaide Research and Scholarship : Schools and Disciplines : School of Earth and Environmental Sciences : Earth and Environmental Sciences publications

Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/74252

Type: Journal article
Title: Description and crystal structure of maghrebite, MgAl₂(AsO₄)₂(OH)₂•8H₂O, from Aghbar, Anti-Atlas, Morocco: first arsenate in the laueite mineral group
Other Titles: Description and crystal structure of maghrebite, MgAl(2)(AsO(4))(2)(OH)(2)(.)8H(2)O, from Aghbar, Anti-Atlas, Morocco: first arsenate in the laueite mineral group
Author: Meisser, Nicolas
Brugger, Joel
Krivovichev, Sergey V.
Armbruster, Thomas
Favreau, Georges
Citation: European Journal of Mineralogy, 2012; 24(4):717-726
Publisher: E Schweizerbartsche Verlags
Issue Date: 2012
ISSN: 0935-1221
School/Discipline: School of Earth and Environmental Sciences
Statement of
Responsibility: 
Nicolas Meisser, Joël Brugger, Sergey Krivovichev, Thomas Armbruster and Georges Favreau
Abstract: Maghrebite, MgAl2(AsO4)2(OH)2•8H2O, is a new mineral occurring at the Aghbar open pit mine, Bou Azzer district, Anti-Atlas, Morocco. Maghrebite is associated with quartz, erythrite, arseniosiderite, wendwilsonite and cabalzarite, and results from the weathering of a Variscan hydrothermalCo-Ni-As-(Cu-U-Mo) vein. Maghrebite forms lozenge-shaped prismatic crystals up to 0.2 mm in length. It is colorless, translucent with vitreous luster. Dmeas is 2.60(1) g/cm3, Dcalc (crystal structure) 2.46 g/cm3. The new mineral is biaxial negative without pleochroism. Measured 2V angle is 87 (3)_; the refractive indices measured at 589 nm are: a ¼ 1.562 (2), b ¼ 1.574 (2), g ¼ 1.586 (2) with the following orientation a // b; b ^ c ¼ 28.8_ and g ^ a ¼ 25.5_. The empirical chemical formula is (Mg0.96Co0.01Ca0.01)P¼0.98(Al1.94Fe3þ 0:06)P¼2.00(As2.01Si0.01)P¼2.02H18.0O18.02. Maghrebite is triclinic, P_1, Z ¼ 1, with a ¼ 5.436 (2)A ° , b ¼ 10.500 (3)A ° , c¼7.075 (2)A ° , a ¼97.701 (7)_, b¼ 110.295 (5)_, g¼ 102.021 (6)_ and V¼ 361.0 (2)A ° 3. The six strongest lines in the X-ray powder diffraction pattern are [d in A ° (I)(hkl)]: 9.9 (100) (010), 6.4 (90) (001), 4.90 (80) (_101), 3.198 (60) (002), 2.885 (60) (_131) and 2.622 (60) (13-1). The structure was solved by direct methods and refined to R1¼0.045 on the basis of 1064 unique observed reflections. The structure is based upon [Al(AsO4)(OH)(H2O)3]_ layers parallel to (010) and interlinked by [Mg(H2O)6]þ octahedra. In addition, there is one H2O molecule in the structure that is not bonded to any cation but is held in between the layers by hydrogen bonds only. The topology of the Al arsenate octahedral-tetrahedral layer is that of the laueite type and belongs to the laueite isomer of the laueite-stewartite-pseudolaueite-metavauxite group of structural and geometrical isomers. Maghrebite is an arsenate analogue of gordonite and is the first natural member of the laueite group to contain arsenate as the major anion group.
Keywords: Maghrebite; new mineral; crystal structure determination; laueite group; arsenic; Aghbar; Anti-Atlas; Morocco
Rights: © 2012 by Schweizerbart science publishers
RMID: 0020121705
DOI: 10.1127/0935-1221/2012/0024-2172
Appears in Collections:Earth and Environmental Sciences publications
View citing articles in: Web of Science
Google Scholar
Scopus

There are no files associated with this item.

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

 

© 2008 The University of Adelaide
library@adelaide.edu.au
CRICOS Provider Number 00123M
Service Charter | Copyright | Privacy | Disclaimer