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- W2034573289 abstract "Lawsonite of early Alpine age formed in different tectonic sub-units of the Sesia zone (western Italian Alps). In the southern part of the “eclogitic micaschists” subunit (EM), lawsonite grew with quartz ± Jadeite during the early Alpine retrograde path which just post-dates the eclogite thermal peak. The early retrograde path of the southern EM occurred at decreasing temperature and at P-T conditions comparable to those of the metamorphic peak in some blueschist facies thrust sheets which separate the EM from the Southern Alps. Such a post-eclogitic cooling path may have been induced by conductive cooling linked to migration of the underthrust surfaces, and to stacking with colder nappes like the other Sesia subunits or the Piemonte metaophiolites. Stacking and thermal interaction between the different units probably occurred at depth, during the early stages of exhumation which followed subduction-underthrusting of early-mid Cretaceous age. During the Paleogene, continental collision between the European and African plates determined further underthrusts of more westerly units; these units underwent a high-pressure, very-low-temperature recrystallization (meso-Alpine event) characterized by the growth of lawsonite at the peak metamorphic conditions. Consequently, propagation of the underthrust surfaces may represent an effective mechanism to prevent the rise of the isotherms and to favor post-peak cooling paths in some units of the Western Alps. This effect is more obvious in the structurally upper units which were first brought to deep crustal levels in the early Alpine imbricated subduction zone." @default.
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- W2034573289 date "1989-05-01" @default.
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- W2034573289 title "Tectonic implications of lawsonite formation in the Sesia zone (Western Alps)" @default.
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- W2034573289 doi "https://doi.org/10.1016/0040-1951(89)90245-x" @default.
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