18 citations as recorded by crossref.

1. Adamastor – an ocean that never existed? J. Konopásek et al. https://doi.org/10.1016/j.earscirev.2020.103201
2. Connecting the Araçuaí and Ribeira belts (SE – Brazil): Progressive transition from contractional to transpressive strain regime during the Brasiliano orogeny M. Egydio-Silva et al. https://doi.org/10.1016/j.jsames.2018.06.005
3. Reconstructing the metamorphic evolution of the Araçuaí orogen (SE Brazil) using in situ U–Pb garnet dating and P–T modelling M. Schannor et al. https://doi.org/10.1111/jmg.12605
4. A critical discussion of the subduction-collision model for the Neoproterozoic Araçuaí-West Congo orogen H. Fossen et al. https://doi.org/10.1016/j.precamres.2020.105715
5. The role of deformation-assisted by water influx on partial melting of a granite protolith, and its role in the evolution of southwestern São Francisco Craton margin, Brazil E. Julião et al. https://doi.org/10.1016/j.jsames.2021.103605
6. Petrologic and geochronological constraints on the polymetamorphic evolution of the collisional granites, Araçuaí Orogen (SE Brazil) S. MAURI et al. https://doi.org/10.1590/0001-3765202120200639
7. How long can the middle crust remain partially molten during orogeny? C. Cavalcante et al. https://doi.org/10.1130/G45126.1
8. The influence of partial melting and melt migration on the rheology of the continental crust G. Cavalcante et al. https://doi.org/10.1016/j.jog.2016.06.002
9. Slow cooling and crystallization of the roots of the Neoproterozoic Araçuaí hot orogen (SE Brazil): Implications for rheology, strain distribution, and deformation analysis A. Vauchez et al. https://doi.org/10.1016/j.tecto.2019.05.013
10. Reviewing the puzzling intracontinental termination of the Araçuaí-West Congo orogenic belt and its implications for orogenic development C. Cavalcante et al. https://doi.org/10.1016/j.precamres.2018.12.025
11. Confronting Episodic vs. Continuous Heat Sources in Long‐Lived Hot Orogens: Insights From Petrochronological Studies in the Nova Venecia Complex, Araçuaí Orogen (SE Brazil) L. Schiavetti et al. https://doi.org/10.1111/jmg.70007
12. Temperature and timing of ductile deformation of the Longquanguan shear zone, Trans-North China Orogen J. Liu et al. https://doi.org/10.1016/j.precamres.2021.106217
13. The role of Ediacaran synkinematic anatectic rocks and the late-orogenic charnockitic rocks in the development of the hot Araçuaí belt C. Cavalcante et al. https://doi.org/10.1016/j.precamres.2021.106396
14. Hot Versus Cold Orogenic Behavior: Comparing the Araçuaí‐West Congo and the Caledonian Orogens H. Fossen et al. https://doi.org/10.1002/2017TC004743
15. Building an inversely zoned post-orogenic intrusion in the Neoproterozoic-Cambrian Araçuaí orogen (Brazil) U. Bellon et al. https://doi.org/10.1016/j.jsg.2021.104401
16. Temperature constraints on microfabric patterns in quartzofeldsphatic mylonites, Ribeira belt (SE Brazil) C. Cavalcante et al. https://doi.org/10.1016/j.jsg.2018.07.013
17. Midcrust deformation regime variations across the Neoproterozoic Araçuaí hot orogen (SE Brazil): Insights from structural and magnetic fabric analyses T. Angelo et al. https://doi.org/10.1016/j.jsg.2020.104007
18. Magnetic Fabric and Geochronology of a Cambrian “Isotropic” Pluton in the Neoproterozoic Araçuaí Orogen F. Temporim et al. https://doi.org/10.1029/2019TC005877