High-pressure granulite-facies metamorphism in central Dronning Maud Land (East Antarctica): Implications for Gondwana assembly

Autor: Palmeri R.[1], Godard G.[2], Di Vincenzo G.[3], Sandroni S. [1], Talarico F. [1

Publikováno v: Lithos (Oslo. Print) 300-301 (2018): 361–377.
info:cnr-pdr/source/autori:Palmeri R.[1], Godard G.[2], Di Vincenzo G.[3], Sandroni S. [1], Talarico F. [1,4]/titolo:High-pressure granulite-facies metamorphism in central Dronning Maud Land (East Antarctica): Implications for Gondwana assembly/doi:/rivista:Lithos (Oslo. Print)/anno:2018/pagina_da:361/pagina_a:377/intervallo_pagine:361–377/volume:300-301

Central Dronning Maud Land (DML; East Antarctica) is located in a key region of the Gondwana supercontinent. The Conradgebirge area (central DML) consists of orthogneisses, derived from both volcanic and plutonic protoliths, and minor metasedimentary

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::7784ccc46cfa7a770e86c1176963caba
https://publications.cnr.it/doc/386547