The Neoproterozoic Agudos Grandes granitic batholith, SE Brazil: Inferences on source areas from elemental and Sr-Nd-Pb isotope geochemistry
Author:
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geology
Reference45 articles.
1. Sources of granite magmatism in the Embu Terrane (Ribeira Belt, Brazil): Neoproterozoic crust recycling constrained by elemental and isotope (Sr-Nd-Pb) geochemistry;Alves;J. S. Am. Earth Sci.,2016
2. Most granitoid rocks are cumulates: deductions from hornblende compositions and zircon saturation;Barnes;J. Petrol.,2020
3. Chemical differentiation by mineralogical buffering in crustal hot zones;Blundy;J. Petrol.,2022
4. The formation of high-Sr/Y plutons in cordilleran-arc crust by crystal accumulation and melt loss;Brackman;Geosphere,2022
5. Petrochronological constraints and tectonic implications of Tonian metamorphism in the Embu complex, Ribeira belt, Brazil;Cabrita;Precambrian Res.,2021
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1. Neoproterozoic High-K calc-alkaline granites forming the large Agudos Grandes and Socorro batholiths, SE Brazil: crystallization conditions and tectonic implications;Journal of South American Earth Sciences;2024-09
2. Passive continental margin subducted to mantle depths: Coesite-bearing metasedimentary rocks from the Neoproterozoic Brasília Orogen, West Gondwana margin;Precambrian Research;2024-08
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