Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Mazzucchelli M.L.[1"'
Publikováno v:
The American mineralogist (Online) 106 (2021): 830–837. doi:10.2138/am-2021-7693
info:cnr-pdr/source/autori:Mazzucchelli M.L.[1,2,3], Angel R.J.[4], Alvaro M.[1]/titolo:EntraPT: An online platform for elastic geothermobarometry/doi:10.2138%2Fam-2021-7693/rivista:The American mineralogist (Online)/anno:2021/pagina_da:830/pagina_a:837/intervallo_pagine:830–837/volume:106
info:cnr-pdr/source/autori:Mazzucchelli M.L.[1,2,3], Angel R.J.[4], Alvaro M.[1]/titolo:EntraPT: An online platform for elastic geothermobarometry/doi:10.2138%2Fam-2021-7693/rivista:The American mineralogist (Online)/anno:2021/pagina_da:830/pagina_a:837/intervallo_pagine:830–837/volume:106
EntraPT is a web-based application for elastic geobarometry freely accessible at the "Fiorenzo Mazzi" experimental mineralogy lab website (http://www.mineralogylab.com/software/). It provides an easy-to-use tool to calculate the entrapment conditions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::46de2f059bbfe7d4d067cb199db5a0d6
http://www.cnr.it/prodotto/i/454315
http://www.cnr.it/prodotto/i/454315
Publikováno v:
Lithos
Lithos (Oslo. Print) 350-351 (2019): 1–10. doi:10.1016/j.lithos.2019.105218
info:cnr-pdr/source/autori:Mazzucchelli M.L.[1], Reali A.[2], Morganti S.[3], Angel R.J.[1,4], Alvaro M.[1]/titolo:Elastic geobarometry for anisotropic inclusions in cubic hosts/doi:10.1016%2Fj.lithos.2019.105218/rivista:Lithos (Oslo. Print)/anno:2019/pagina_da:1/pagina_a:10/intervallo_pagine:1–10/volume:350-351
Lithos (Oslo. Print) 350-351 (2019): 1–10. doi:10.1016/j.lithos.2019.105218
info:cnr-pdr/source/autori:Mazzucchelli M.L.[1], Reali A.[2], Morganti S.[3], Angel R.J.[1,4], Alvaro M.[1]/titolo:Elastic geobarometry for anisotropic inclusions in cubic hosts/doi:10.1016%2Fj.lithos.2019.105218/rivista:Lithos (Oslo. Print)/anno:2019/pagina_da:1/pagina_a:10/intervallo_pagine:1–10/volume:350-351
Mineral inclusions entrapped in other minerals may record the local stresses at the moment of their entrapment in the deep Earth. When rocks are exhumed to the surface of the Earth, residual stresses and strains may still be preserved in the inclusio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a82f23dc13825198918579a9336a64bd
