The composition of peridotite tectonites from the Ivrea Complex, northern Italy - Residues from melt extraction

Details The composition of peridotite tectonites from the Ivrea Complex, northern Italy - Residues from melt extraction The composition of peridotite tectonites from the Ivrea Complex, northern Italy - Residues from melt extraction

Apr 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993gecoa..57.1761h&link_type=abstract

Geochimica et Cosmochimica Acta (ISSN 0016-7037), vol. 57, no. 8, p. 1761-1782.

Computer Science

9

Chemical Composition, Mineralogy, Oxygen 18, Peridotite, Strontium Isotopes, Earth Crust, Earth Mantle, Italy, Spinel

Scientific paper

Results are presented of analyses of forty-three samples from three peridotite tectonites (Balmuccia, Baldissero, and Finero) from the Ivrea Complex (northern Italy) for major elements, forty minor elements, and mineral composition. A subset of samples was also investigated with respect to delta D, delta (O-18), delta (S-34), and Sr-87/Sr-86 ratios. The results disagree with the report of Ernst (1978) on Al and on modal compositions in peridotites from the same localities. The nature of the three samples from the Balmuccia/Baldissero and Finero is discussed.

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