Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/4834
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dc.contributor.authorallIezzi, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallLiu, Z.en
dc.contributor.authorallDella Ventura, G.en
dc.date.accessioned2008-12-16T07:26:30Zen
dc.date.available2008-12-16T07:26:30Zen
dc.date.issued2009-
dc.identifier.urihttp://hdl.handle.net/2122/4834en
dc.description.abstracthigh-pressure behavior of three synthetic amphiboles crystallized with space group P21/m at room conditions in the system Li2O–Na2O–MgO–SiO2–H2O has been studied by in situ synchrotron infrared absorption spectroscopy. The amphiboles have compositions ANa B(NaxLi1 ¡ xMg1) CMg5 Si8 O22(OH)2 with x = 0.6, 0.2 and 0.0, respectively. The high-P experiments up to 32 GPa were carried out on the U2A beamline at Brookhaven National Laboratory (NY, USA) using a diamond anvil cell under non-hydrostatic or quasi-hydrostatic conditions. The two most intense absorption bands in the OH-stretching infrared spectra can be assigned to two non-equivalent O–H dipoles in the P21/m structure, bonded to the same local environment M1M3Mg3–OH–ANa, and pointing toward two diVerently kinked tetrahedral rings. In all samples these bands progressively merge to give a unique symmetrical absorption with increasing pressure, suggesting a change in symmetry from P21/m to C2/m. The pressure at which the transition occurs appears to be linearly correlated to the aggregate B-site dimension. The infrared spectra collected for amphibole B(Na0.2Li0.8Mg1) in the frequency range 50 to 1,400 cm¡1 also show a series of changes with increasing pressure. The data reported here support the inference of Iezzi et al. (Am Miner 91:479–482, 2006a) regarding a new high-pressure C2/m amphibole polymorph characterized by two equivalent and kinked double-chains, stable at very high-pressure.en
dc.language.isoEnglishen_US
dc.publisher.nameSpringeren_US
dc.relation.ispartofPhysics and Chemistry of Mineralsen_US
dc.relation.ispartofseries/36 (2009)en_US
dc.relation.isversionofhttp://www.springerlink.com/content/100449/?p=9ed04048f0984ce0b83071cf68db968a&pi=39en_US
dc.subjectHigh-pressureen
dc.subjectB-site dimensionen
dc.titleSynthetic ANaB(NaxLi1 ¡ xMg1)CMg5Si8O22(OH)2 (with x = 0.6, 0.2 and 0) P21/m amphiboles at high pressure: a synchrotron infrared studyen_US
dc.typearticleen
dc.description.statusPublisheden_US
dc.type.QualityControlPeer-revieweden_US
dc.description.pagenumber343–354en_US
dc.subject.INGV04. Solid Earth::04.01. Earth Interior::04.01.04. Mineral physics and properties of rocksen
dc.identifier.doi10.1007/s00269-008-0282-yen_US
dc.description.obiettivoSpecifico2IT. Laboratori analitici e sperimentalien_US
dc.description.journalTypeJCR Journalen_US
dc.description.fulltextreserveden
dc.contributor.authorIezzi, G.-
dc.contributor.authorLiu, Z.-
dc.contributor.authorDella Ventura, G.-
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen_US
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità degli studi G. D'annunzio, Chieti Pescara, Italy-
crisitem.author.deptDipartimento di Scienze Geologiche Università Roma Tre-
crisitem.author.orcid0000-0001-6277-961X-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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