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The magnetite ore districts of the southern Aosta Valley (Western Alps, Italy): a mineralogical study of metasomatized chromite ore

Published online by Cambridge University Press:  05 July 2018

P. Rossetti ,
G. D. Gatta ,
V. Diella ,
S. Carbonin ,
A. Della Giusta  and
A. Ferrario
P. Rossetti
Affiliation:
Dipartimento di Scienze Mineralogiche e Petrologiche, Università degli Studi di Torino, Italy
G. D. Gatta*
Affiliation:
Dipartimento di Scienze della Terra, Università degli Studi di Milano, Italy CNR-Istituto per la Dinamica dei Processi Ambientali, Milano, Italya
V. Diella
Affiliation:
CNR-Istituto per la Dinamica dei Processi Ambientali, Milano, Italya
S. Carbonin
Affiliation:
Dipartimento di Geoscienze, Università degli Studi di Padova, Italy
A. Della Giusta
Affiliation:
Dipartimento di Geoscienze, Università degli Studi di Padova, Italy
A. Ferrario
Affiliation:
Dipartimento di Geoscienze, Università degli Studi di Padova, Italy
*
* E-mail: [email protected]
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Abstract

In the southern Aosta Valley (Italian Western Alps), several massive magnetite bodies occur within serpentinized ultramafic rocks belonging to the Mesozoic meta-ophiolite nappe. The ultramafic rocks consist of lherzolite with minor dunite bodies and show a high pressure metamorphic overprint. The results of a multi-methodological study, based on optical microscopy, electron microprobe analysis and single-crystal X-ray diffraction, are reported here in order to give new insights into (1) the mineralogy and crystal chemistry of spinels and silicates and (2) the genesis of the massive magnetite bodies. Chromium-rich relict cores inside the magnetite grains suggest a derivation from primary chromite concentrations. The major-element behaviour shows the presence of two chromite types: a Cr2O3-rich (Al2O3-poor) type and a Cr2O3-poor (Al2O3-rich) type. Magnetite ore deposits probably represent the product of transformation from a chromite proto-ore which formed in ultramafic rocks pertaining to an ophiolite suite. The transformation of chromite to magnetite occurred during multiple stages: the pre- metamorphic setting of the ultramafics and the petrographic evidence suggest that metasomatism started before the onset of the alpine metamorphism and was active during the early alpine, eclogite- facies metamorphic overprint related to a subduction process under high fluid activity.

Keywords

chromitemagnetiteserpentinizationhigh pressureocean floormetasomatismPiemonte Zone.
Type
Research Article
Information
Mineralogical Magazine , Volume 73 , Issue 5 , October 2009 , pp. 737 - 751
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2009

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