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Publikováno v:
Journal of Geodinamics. 43 (2007): 465–483. doi:10.1016/j.jog.2006.11.002
info:cnr-pdr/source/autori:Corti G.[1], Bonini M.[1], Innocenti F.[2,3], Manetti P.[2], Piccardo G.B.[4], Ranalli G.[5]/titolo:Experimental models of extension of continental lithosphere weakened by percolation of sthenospheric melts/doi:10.1016%2Fj.jog.2006.11.002/rivista:Journal of Geodinamics./anno:2007/pagina_da:465/pagina_a:483/intervallo_pagine:465–483/volume:43
info:cnr-pdr/source/autori:Corti G.[1], Bonini M.[1], Innocenti F.[2,3], Manetti P.[2], Piccardo G.B.[4], Ranalli G.[5]/titolo:Experimental models of extension of continental lithosphere weakened by percolation of sthenospheric melts/doi:10.1016%2Fj.jog.2006.11.002/rivista:Journal of Geodinamics./anno:2007/pagina_da:465/pagina_a:483/intervallo_pagine:465–483/volume:43
Analogue models are used to investigate extension of a continental lithosphere weakened by asthenospheric melts percolating through the upper mantle, a process that has been hypothesised to control the opening of the Ligurian Tethys. Models were perf