V. Meira

发表

LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile

C. Hall, C. Juliani, A. Garcia‐Casco, 2015 .

A Neoproterozoic hyper-extended margin associated with Rodinia's demise and Gondwana's build-up: The Araguaia Belt, central Brazil

C. Lana, M. Macouin, M. Rospabé, 2019, Gondwana Research.

Ordovician klippen structures of the Sierra de Umango: New insights on Tectonic evolution of the Western Sierras Pampeanas, Argentina

M. Basei, R. Varela, V. Meira, 2012 .

Accretion of Grenvillian terranes to the southwestern border of the Río de la Plata craton, western Argentina

M. Basei, R. Varela, M. Naipauer, 2011 .

The role of Ediacaran synkinematic anatectic rocks and the late-orogenic charnockitic rocks in the development of the hot Araçuaí belt

C. Cavalcante, M. Hollanda, V. Meira, 2021, Precambrian Research.

Long-lived intracontinental deformation associated with high geothermal gradients in the Seridó Belt (Borborema Province, Brazil)

A. Gerdes, P. Lanari, R. Trindade, 2021 .

The role of intracontinental deformation in supercontinent assembly: insights from the Ribeira Belt, Southeastern Brazil (Neoproterozoic West Gondwana)

C. Juliani, A. Garcia‐Casco, R. P. Almeida, 2015 .

Reply to Comment by Heilbron and Valeriano on “Tectono Metamorphic Evolution of the Central Ribeira Belt, Brazil: A Case of Late Neoproterozoic Intracontinental Orogeny and Flow of Partially Molten Deep Crust During the Assembly of West Gondwana”

C. Juliani, A. Garcia‐Casco, T. Hyppolito, 2020, Tectonics.

A critical discussion of the subduction-collision model for the Neoproterozoic Araçuaí-West Congo orogen

R. D. de Almeida, H. Fossen, C. Cavalcante, 2020 .

Spinel-group minerals as a record of magmatic and metamorphic processes: evidence from the highly altered Morro do Onça ultramafic suite, São Francisco Craton (Brazil)

Marco Aurélio Piacentini Pinheiro, Raianny Carolini Ramos Ferreira, V. Meira, 2022, Contributions to Mineralogy and Petrology.

Late Tonian within-plate mafic magmatism and Ediacaran partial melting and magmatism in the Costeiro Domain, Central Ribeira Belt, Brazil

C. Juliani, A. Garcia‐Casco, V. Meira, 2019, Precambrian Research.

Tectono‐Metamorphic Evolution of the Central Ribeira Belt, Brazil: A Case of Late Neoproterozoic Intracontinental Orogeny and Flow of Partially Molten Deep Crust During the Assembly of West Gondwana

C. Juliani, A. Garcia‐Casco, T. Hyppolito, 2019, Tectonics.

Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): Counterclockwise P-T paths and timing of metamorphism of deep-seated garnet-mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S)

C. Juliani, A. Garcia‐Casco, C. Hall, 2014 .

The nature of the Palaeozoic oceanic basin at the southwestern margin of Gondwana and implications for the origin of the Chilenia terrane (Pichilemu region, central Chile)

C. Juliani, A. Garcia‐Casco, F. Hervé, 2014 .

Reassessment of Aguapeí (Salto do Céu) paleomagnetic pole, Amazonian Craton and implications for Proterozoic supercontinents

R. Trindade, L. Janikian, V. Meira, 2016 .

Comment to “Neoproterozoic magmatic arc systems of the central Ribeira belt, SE-Brazil, in the context of the West-Gondwana pre-collisional history: A review”

H. Fossen, C. Cavalcante, V. Meira, 2020 .

Supplemental Material: Metamorphism of the Sierra de Maz and implications for the tectonic evolution of the MARA terrane

J. Vervoort, W. McClelland, M. Coble, 2021, Geosphere.