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

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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:2022 Issue: Volume: Page:
ISSN:1556-5068
Container-title:SSRN Electronic Journal
language:en
Short-container-title:SSRN Journal

Author:

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

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference118 articles.

1. Ossa-Morena Zone: Structure;O Apalategui;Pre-Mesozoic Geology of Iberia,1990

2. Implica��es na evolu��o geodin�mica da margem Sudoeste do Terreno Aut�ctone Ib�rico;A Ara�jo;Estrutura de uma Geotransversal entre Brinches e Mour�o,1995

3. The Moura Phyllonitic Complex: An Accretionary Complex related with obduction in the Southern Iberia Variscan Suture;A Ara�jo;Geodinamica Acta, v,2005

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;J C S Ara�jo;Journal of South American Earth Sciences,2019

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