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Publikováno v:
Journal of petrology
58 (2017): 599–640. doi:10.1093/petrology/egx028
info:cnr-pdr/source/autori:Marchev P.[1], Arai S.[2], Vaselli O.[3,4], Costa F. [5], Zanetti A.[6], Downes H. [7]/titolo:Metasomatic reaction phenomena from entrainment to surface cooling: Evidence from mantle peridotite xenoliths from Bulgaria/doi:10.1093%2Fpetrology%2Fegx028/rivista:Journal of petrology (Print)/anno:2017/pagina_da:599/pagina_a:640/intervallo_pagine:599–640/volume:58
58 (2017): 599–640. doi:10.1093/petrology/egx028
info:cnr-pdr/source/autori:Marchev P.[1], Arai S.[2], Vaselli O.[3,4], Costa F. [5], Zanetti A.[6], Downes H. [7]/titolo:Metasomatic reaction phenomena from entrainment to surface cooling: Evidence from mantle peridotite xenoliths from Bulgaria/doi:10.1093%2Fpetrology%2Fegx028/rivista:Journal of petrology (Print)/anno:2017/pagina_da:599/pagina_a:640/intervallo_pagine:599–640/volume:58
We present a detailed study of the mineralogical and chemical modifications of peridotite xenoliths during magma transport and cooling at the Earth's surface. The xenoliths are entrained in three small-volume (