Skip to main navigation Skip to search Skip to main content

Subduction-related melt refertilisation and alkaline metasomatism in the Eastern Transylvanian Basin lithospheric mantle: Evidence from mineral chemistry and noble gases in fluid inclusions

  • Barbara Faccini
  • , Andrea Luca Rizzo
  • , Costanza Bonadiman
  • , Theodoros Ntaflos
  • , Ioan Seghedi
  • , Michel Gregoire
  • , Giacomo Ferretti
  • , Massimo Coltorti

Publications: Contribution to journalArticlePeer Reviewed

Original languageEnglish
Article number105516
Number of pages24
JournalLithos
Volume364-365
DOIs
Publication statusPublished - Jul 2020

Funding

The project was funded by the Italian National Research Program PRIN_2017 Project 20178LPCPWand PRIN_2017 Project 2017LMNLAW to M.C. and A.L.R., respectively. The noble gas contribution in this work is part of the PhD (XXXII cycle) of A. L. R. at the University of Ferrara. We thank Mariagrazia Misseri and Mariano Tantillo for helping in samples preparation, isotope analysis of noble gases and laboratory activities. I.S. was supported by grant of Ministry of Research and Innovation, CNCS -UEFISCDI, project number PN-III-P4-ID-PCCF-2016-4-0014, within PNCDI III. Helpful suggestions by Hilary Downes and an anonymous reviewer greatly improved the manuscript.

Austrian Fields of Science 2012

  • 105105 Geochemistry
  • 105120 Petrology

Keywords

  • Mantle refertilisation
  • Eastern Transylvanian Basin
  • Noble gases
  • Post-collisional
  • Subduction-related metasomatism
  • CARPATHIAN-PANNONIAN REGION
  • TRACE-ELEMENT COMPOSITIONS
  • SUB-ARC MANTLE
  • PERIDOTITE XENOLITHS
  • SUBCONTINENTAL MANTLE
  • ABYSSAL PERIDOTITES
  • AVACHA VOLCANO
  • COMPOSITIONAL VARIATIONS
  • OXIDATION-STATE
  • ORTHO-PYROXENE

Fingerprint

Dive into the research topics of 'Subduction-related melt refertilisation and alkaline metasomatism in the Eastern Transylvanian Basin lithospheric mantle: Evidence from mineral chemistry and noble gases in fluid inclusions'. Together they form a unique fingerprint.

Cite this