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Low-T neutron powder-diffraction and synchrotron-radiation IR study of synthetic amphibole Na(NaMg)Mg (sub 5) Si (sub 8) O (sub 22) (OH) (sub 2)

G. Iezzi, G. D. Gatta, W. Kockelmann, G. Della Ventura, R. Rinaldi, W. Schaefer, M. Piccinini and F. Gaillard
Low-T neutron powder-diffraction and synchrotron-radiation IR study of synthetic amphibole Na(NaMg)Mg (sub 5) Si (sub 8) O (sub 22) (OH) (sub 2) (in Monazite microprobe geochronology, Michael L. Williams (prefacer) and Robert J. Tracy (prefacer))
American Mineralogist (April 2005) 90 (4): 695-700

Abstract

(super A) Na (super B) (NaMg) (super C) Mg (sub 5) Si (sub 8) O (sub 22) (OH,D) (sub 2) amphibole was hydrothermally synthesized at 850 degrees C and 0.3 GPa. SEM, EPMA, and X-ray powder-diffraction data showed the experimental product to consist of a high amphibole yield (90-95%), plus minor quartz and rare enstatite. Neutron powder-diffraction data were collected using a time-of-flight diffractometer at room T and at 8 K, respectively, and structure refinement was carried out using the Rietveld method. The space group of the amphibole is P2 (sub 1) /m at both temperatures, as confirmed by the presence of b-type reflections (h + k = 2n + 1). FTIR OH- and OD-stretching spectra at both room and low T (30 K) show two main absorptions, which are assigned to two non-equivalent OH groups in the structure, and a third lower-frequency band, assigned to A-site vacant environments (local cummingtonite environments). At room- and low-T, the cell parameters are (in Aa): a 9.7188(1) and 9.7016(2), b 17.9385(3) and 17.8953(4), c 5.2692(1) and 5.2574(1); beta ( degrees ) is 102.526(1) and 102.597(2). Cell volumes (Aa (super 3) ) are 896.78(2) at room T and 890.80(2) at 8 K, with a relative reduction of less than 1%. Accurate structural positions for the hydrogen atoms were obtained from diffraction data. The O5A-O6A-O5A and O5B-O6B-O5B angles, diagnostic of the A- and B-chains kinking along c, are 190.0 degrees and 159.2 degrees at 293 K and 193.8 degrees and 156.8 degrees at 8 K, respectively. The orientation of the thermoelastic strain ellipsoid was calculated and the principal unit-strain tensor components are reported. A comparison between the low-temperature data reported here and the high-temperature data for a similar amphibole composition, reported by Camara et al. (2003) up to 643 K, is discussed.


ISSN: 0003-004X
EISSN: 1945-3027
Coden: AMMIAY
Serial Title: American Mineralogist
Serial Volume: 90
Serial Issue: 4
Title: Low-T neutron powder-diffraction and synchrotron-radiation IR study of synthetic amphibole Na(NaMg)Mg (sub 5) Si (sub 8) O (sub 22) (OH) (sub 2)
Title: Monazite microprobe geochronology
Author(s): Iezzi, G.Gatta, G. D.Kockelmann, W.Della Ventura, G.Rinaldi, R.Schaefer, W.Piccinini, M.Gaillard, F.
Author(s): Williams, Michael L.prefacer
Author(s): Tracy, Robert J.prefacer
Affiliation: Universitaet Bayreuth, Bayerisches Geoinstitut, Bayreuth, Federal Republic of Germany
Affiliation: University of Massachusetts, Department of Geosciences, Amherst, MA, United States
Pages: 695-700
Published: 200504
Text Language: English
Publisher: Mineralogical Society of America, Washington, DC, United States
Meeting name: Geological Society of America annual meeting
Meeting location: Denver, CO, USA, United States
Meeting date: 20021027Oct. 27-30, 2002
References: 18
Accession Number: 2005-035154
Categories: Mineralogy of silicates
Document Type: Serial Conference document
Bibliographic Level: Analytic
Illustration Description: illus. incl. 4 tables
Secondary Affiliation: Virginia Polytechnic Institute and State University, USA, United StatesRutherford Appleton, GBR, United KingdomUniversita di Roma Tre, ITA, ItalyForschungszentrum Juelich, DEU, Federal Republic of GermanyI.N.F.N., Laboratori Nazionali di Frascati, ITA, Italy
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 200520
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