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Publikováno v:
Lithos (Oslo. Print) 392-393 (2021): 1–23. doi:10.1016/j.lithos.2021.106129
info:cnr-pdr/source/autori:Benetti B.[1], Montomoli C.[1,2], Iaccarino S.[1], Langone A.[3], Carosi R.[1]/titolo:Mapping tectono-metamorphic discontinuities in orogenic belts: implications for mid-crust exhumation in NW Himalaya/doi:10.1016%2Fj.lithos.2021.106129/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:23/intervallo_pagine:1–23/volume:392-393
info:cnr-pdr/source/autori:Benetti B.[1], Montomoli C.[1,2], Iaccarino S.[1], Langone A.[3], Carosi R.[1]/titolo:Mapping tectono-metamorphic discontinuities in orogenic belts: implications for mid-crust exhumation in NW Himalaya/doi:10.1016%2Fj.lithos.2021.106129/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:23/intervallo_pagine:1–23/volume:392-393
A newly identified high-temperature shear zone, the Badrinath shear zone (BSZ), is described within the metamorphic core of the Himalayan belt along the Alaknanda valley, Garhwal Himalaya (NW India). A multidisciplinary approach comprising fieldwork,