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Constraints on F vs. OH incorporation in synthetic [6]Al-bearing monoclinic amphiboles

Giancarlo Della Ventura 1 Jean-Louis Robert 2 José Sergent 2 Franck C. Hawthorne 3 François Delbove 2
1 Dipartimento di Scienze Geologiche [Roma TRE]
2 ISTO - Institut des Sciences de la Terre d'Orléans
3 DEPARTMENT OF GEOLOGICAL SCIENCES - Department of Geological Sciences
Abstract : In this work we have systematically replaced OH with F in an amphibole composition intermediate between richterite and pargasite [60% richterite and 40% pargasite in molar proportion; nominal composition Na(Na0.6Ca1.4)(Mg4.6Al0.4)(Si7.2Al0.8)O22(OH,F)2]. Syntheses have been done at 3 kbar PH2O and 900 °C, and for all compositions an assemblage of amphibole plus minor Na-phlogopite has been obtained. Crystal-chemical variations in the amphibole as a function of F have been characterized by a combination of EMPA, X-ray powder diffraction, and infrared spectroscopy. EMPA analyses show that for increasing F in the system (i) the [6]Al content decreases to 0.13 apfu for the nominal fluorine end-member whereas the [4]Al content is virtually constant and close to the nominal value; (ii) the fluorine content is systematically lower than expected. The infrared OH-stretching spectra show that those OH-groups locally bonded to M1MgM1MgM3Mg configurations are preferentially replaced by F whereas those OH-groups locally bonded to M1MgM1MgM3Al configurations are not replaced by F.
Keywords : RICHTERITE PARGASITE EMPA CELL PARAMETERS INFRARED SPECTROSCOPY OH-F INCORPORATION
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https://hal-insu.archives-ouvertes.fr/hal-00089722
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Submitted on : Tuesday, August 22, 2006 - 3:41:04 PM
Last modification on : Thursday, October 8, 2020 - 8:40:04 AM

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Giancarlo Della Ventura, Jean-Louis Robert, José Sergent, Franck C. Hawthorne, François Delbove. Constraints on F vs. OH incorporation in synthetic [6]Al-bearing monoclinic amphiboles. European Journal of Mineralogy, Copernicus, 2001, 13, pp.841-847. ⟨10.1127/0935-1221/2001/0013/0841⟩. ⟨hal-00089722⟩

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