Combining δ18O isotope data and in-situ LA-ICP-MS trace element analysis of magnetite as a proxy for ore genesis: Constraints on the formation of Fe deposits from Ossa-Morena Zone (SW Iberian Peninsula)-Reference-Cited by-同舟云学术

Combining δ18O isotope data and in-situ LA-ICP-MS trace element analysis of magnetite as a proxy for ore genesis: Constraints on the formation of Fe deposits from Ossa-Morena Zone (SW Iberian Peninsula)

Published:2023-02 Issue: Volume:245 Page:107140
ISSN:0375-6742
Container-title:Journal of Geochemical Exploration
language:en
Short-container-title:Journal of Geochemical Exploration

Author:

Maia Miguel,Barrulas Pedro,Nogueira Pedro,Mirão José,Noronha Fernando

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology

Reference114 articles.

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4. Depositional model for banded iron formation host to gold in the Archean Rio das Velhas greenstone belt, Brazil, based on geochemistry and LA-ICPMS magnetite analyses;Araújo;J. S. Am. Earth Sci.,2019

5. The Moura Phyllonitic complex: an Accretionary complex related with obduction in the Southern Iberia Variscan Suture;Araújo;Geodin. Acta,2005

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1. Tracing the genesis of the Zhibula skarn deposit, Tibet, using Co, Te, Au and Ag occurrence;Ore Geology Reviews;2023-09

2. Magnetite Talks: Testing Machine Learning Models to Untangle Ore Deposit Classification—A Case Study in the Ossa-Morena Zone (Portugal, SW Iberia);Minerals;2023-07-29