The role of trace element partitioning between garnet, zircon and orthopyroxene on the interpretation of zircon U-Pb ages: an example from high

Autor: Fornelli A.[1], Langone A.[2], Micheletti F.[1], Pascazio A.[1], Piccarreta G.[1]

Publikováno v: International journal of earth sciences (1999, Print) 103 (2014): 487–507. doi:10.1007/s00531-013-0971-8
info:cnr-pdr/source/autori:Fornelli A.[1], Langone A.[2], Micheletti F.[1], Pascazio A.[1], Piccarreta G.[1]/titolo:The role of trace element partitioning between garnet, zircon and orthopyroxene on the interpretation of zircon U-Pb ages: an example from high-.../doi:10.1007%2Fs00531-013-0971-8/rivista:International journal of earth sciences (1999, Print)/anno:2014/pagina_da:487/pagina_a:507/intervallo_pagine:487–507/volume:103

The recognition of the coeval growth of zircon, orthopyroxene and garnet domains formed during the same metamorphic cycle has been attempted with detailed microanalyses coupled with textural analyses. A coronitic garnet-bearing granulite from the low

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::529f6d7b516396ac6fb0bfab2a7ff257
https://publications.cnr.it/doc/285997