Melt migration and melt-rock reaction in the Alpine-Apennine peridotites: Insights on mantle dynamics in extending lithosphere
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DOI: 10.1016/j.gsf.2018.11.001
Abstract: Abstract The compositional variability of the lithospheric mantle at extensional settings is largely caused by the reactive percolation of uprising melts in the thermal boundary layer and in lithospheric environments. The Alpine-Apennine (A-A) ophiolites are… read more here.
Keywords: migration; melt migration; melt rock; alpine apennine ... See more keywords