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MANTLE PROCESSES DURING OCEAN FORMATION: PETROLOGIC RECORDS IN PERIDOTITES FROM THE ALPINE APENNINE OPHIOLITES (2003)
Mantle peridotites were early exposed at the sea-floor of the Jurassic Tethys derived from the subcontinental mantle of the Europe-Adria system. During continental rifting and oceanic spreading, these lithospheric peridotites were percolated via diffuse reactive porous flow by melt fractions produced by near-fractional melting of the upwelling asthenosphere.
Reference:
32nd International Geological Congress Episodes, Vol. 26, no. 3
32nd International Geological Congress Episodes, Vol. 26, no. 3
Organization:
Dept. for the Study of the Territory and Resources, University of Genova, Italy
Italy
Dept. for the Study of the Territory and Resources, University of Genova, Italy
Italy
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