Sources, evolution and ages of A-type granites from the post-orogenic Itu batholith, SE Brazil: Inferences from zircon U–Pb dating, Lu–Hf isotope ratios and trace-element geochemistry-Reference-Cited by-同舟云学术

Sources, evolution and ages of A-type granites from the post-orogenic Itu batholith, SE Brazil: Inferences from zircon U–Pb dating, Lu–Hf isotope ratios and trace-element geochemistry

Published:2023-11 Issue: Volume:131 Page:104619
ISSN:0895-9811
Container-title:Journal of South American Earth Sciences
language:en
Short-container-title:Journal of South American Earth Sciences

Author:

Pereira Giovanna de Souza,Janasi Valdecir de Assis^ORCID,Andrade Sandra,Alves Adriana,Hernandez Viviana Marcela Monsalve

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference39 articles.

1. Tracking the oxygen fugacity of enclave-forming granitic melts through plagioclase trace element signatures;Alves;Contrib. Mineral. Petrol.,2020

2. The origin of felsic microgranitoid enclaves: insights from plagioclase crystal size distributions and thermodynamic models;Alves;Lithos,2015

3. Unravelling the hidden evidences of magma mixing processes via combination of in situ Sr isotopes and trace elements analyses on plagioclase crystals;Alves;Lithos,2021

4. Inhandjara topaz leucogranite: a late rare metal-mineralized stock within the A-type Itu batholith, SE Brazil;Araujo;J. S. Am. Earth Sci.,2020

5. Improved 206Pb/238U microprobe geochronology by the monitoring of a trace-element-related matrix effect; SHRIMP, ID-TIMS, ELA-ICP-MS and oxygen isotope documentation for a series of zircon standards;Black;Chem. Geol.,2004

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