J. B. Silva

发表

Zircon U–Pb geochronology of paragneisses and biotite granites from the SW Iberian Massif (Portugal): evidence for a palaeogeographical link between the Ossa–Morena Ediacaran basins and the West African craton

M. Chichorro, I. Williams, M. F. Pereira, 2008 .

Early Cambrian granitoids of North Gondwana margin in the transition from a convergent setting to intra-continental rifting (Ossa-Morena Zone, SW Iberia)

M. Chichorro, A. R. Solá, M. F. Pereira, 2014, International Journal of Earth Sciences.

Detrital zircon provenance of Triassic sandstone of the Algarve Basin (SW Iberia): evidence of Gondwanan- and Laurussian-type sources of sediment

Q. Crowley, M. F. Pereira, J. B. Silva, 2020, Geological Magazine.

Development of local orthorhombic fabrics within a simple-shear dominated sinistral transpression zone: the Arronches sheared gneisses (Iberian Massif, Portugal)

M. F. Pereira, J. B. Silva, 2004, Geological Society, London, Special Publications.

Variability over time in the sources of South Portuguese Zone turbidites: evidence of denudation of different crustal blocks during the assembly of Pangaea

C. Ribeiro, K. Drost, U. Linnemann, 2014, International Journal of Earth Sciences.

Transcurrent continental tectonics model for the Ossa-Morena Zone Neoproterozoic–Paleozoic evolution, SW Iberian Massif, Portugal

J. B. Silva, M. F. Pereira, 2004 .

The multistage crystallization of zircon in calc-alkaline granitoids: U–Pb age constraints on the timing of Variscan tectonic activity in SW Iberia

P. Moita, R. Armstrong, I. Williams, 2015, International Journal of Earth Sciences.

Early carboniferous wrenching, exhumation of high-grade metamorphic rocks and basin instability in SW Iberia: Constraints derived from structural geology and U–Pb and 40Ar–39Ar geochronology

M. Chichorro, I. Williams, James K. W. Lee, 2012 .

Internal Structure of the Évora Massif: The Évora High-grade Terrains and the Montemor-o-Novo Shear Zone (Ossa-Morena Zone Portugal)

M. Chichorro, M. F. Pereira, J. B. Silva, 2002 .

Genesis of the Ibero-Armorican arc

J. B. Silva, A. Ribeiro, Raphael Antônio do Prado Dias, 1995 .

Comment on Baltic provenance of top-Famennian siliciclastic material of the northern Rhenish Massif, Rhenohercynian zone of the Variscan orogen, by Koltonik et al., International Journal of Earth Sciences (2018) 107:2645–2669

M. F. Pereira, J. B. Silva, C. Gama, 2019, International Journal of Earth Sciences.

Magnetotelluric Imaging of the Lithosphere Across the Variscan Orogen (Iberian Autochthonous Domain, NW Iberia)

F. A. Monteiro-Santos, M. F. Pereira, J. B. Silva, 2017 .

A new model for the Hercynian Orogen of Gondwanan France and Iberia: discussion

M. F. Pereira, J. B. Silva, 2001 .

Terranes within the Iberian Massif: Correlations with West African Sequences

A. Pérez-Estaún, A. Ribeiro, C. Quesada, 1991 .

Structure of the South Portuguese Zone

J. B. Silva, A. Ribeiro, 1983 .

Crustal growth and deformational processes in the northern Gondwana margin: Constraints from the Évora Massif (Ossa-Morena zone, southwest Iberia, Portugal)

P. Moita, M. Chichorro, M. F. Pereira, 2007 .

The role of bedding in the formation of fault–fold structures, Portalegre‐Esperança transpressional shear zone, SW Iberia

J. B. Silva, M. Pereira, C. Ribeiro, 2010 .

The role of strain localization in magma injection into a transtensional shear zone (Variscan belt, SW Iberia)

M. Chichorro, M. F. Pereira, J. B. Silva, 2013, Journal of the Geological Society.

Sinistrai transcurrent transpression at the Ossa-Morena Zone / Central-lberian Zone boundary: the Portalegre-Esperanga shear zone (Portugal)

M. F. Pereira, J. B. Silva, 2000 .