The behaviour of the upper mantle sulfide component during the incipient alteration of ?Alpine?-type peridotites as illustrated by the Beni Bousera (northern Morocco) and Ronda (southern Spain) ultramafic bodies

Author:

Lorand J. P.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference38 articles.

1. Abrajano, T. A., Pasteris, J. D., 1984: The stabilization of native iron and iron-alloys (NIIA) during hydratation of ultramafic rocks. E.O.S.65, 1123.

2. Ahmed, Z., Hall, A., 1982: Nickeliferous opaque minerals associated with chromite alteration in the Sakhakot Qila complex, and their compositional variation. Lithos15, 39?47.

3. Ashley, P. M., 1975: Opaque mineral assemblages formed during serpentinization in the Coolac ultramafic belt, New South Wales. J. Geol. Soc. Australia22, 320?326.

4. Barrakad, A., 1971: Mauchérite et cuivre natif dans les Beni Bousera (Rif Maroc). Notes Serv. geol. Maroc.31, no 237, 285?288.

5. Besson, M., 1975: Les sulfures des lherzolites et ariègites. Bull. Soc. Fr. Min. Crist.98, 53?44.

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