Publications

Filter by type:
(2019). Tangled up in folds: tectonic significance of superimposed folding at the core of the Central Iberian curve (West Iberia). International Geology Review, 61:2, 240-255.

PDF DOI Link

(2018). Late Paleozoic Iberian Orocline(s) and the Missing Shortening in the Core of Pangea. Paleomagnetism From the Iberian Range. Tectonics, 37, 3877–3892.

PDF DOI Link

(2018). Quantifying Arabia–Eurasia convergence accommodated in the Greater Caucasus by paleomagnetic reconstruction. EPSL, 482, 454-469.

PDF DOI Link

(2017). Progressive orocline formation in the Eastern Pontides–Lesser Caucasus. GSLSP, 428.

PDF DOI Link

(2017). Paleomagnetism in Extremadura (Central Iberian Zone, Spain). Journal of Iberian Geology, 43, 4, 583–600.

PDF DOI Link

(2017). Bootstrapped Total Least Squares orocline test: A robust method to quantify vertical axis rotation patterns in orogens, with examples from the Cantabrian and Aegean oroclines. Lithosphere (2017) 9 (3): 499-511.

PDF DOI Link

(2017). Remagnetization during orocline formation. A Carboniferous tale from the Iberian peninsula. Poster from JpGU2017.

Poster

(2016). Paleomagnetism of the Central Iberian bend's hinge: too many oroclines in the Iberian variscides. Gondwana Research.

PDF DOI Link

(2016). Paleomagnetism.org: an online multi-platform open source environment for paleomagnetic data analysis. Computers and Geosciences, 93, 127-137.

PDF DOI Link

(2016). New kinematic constraints on the Ibero-Armorican orocline: a paleomagnetic study from the Peñalba syncline and the Truchas Synform, NW Spain. Tectonophysics, 681, 195–208.

PDF DOI Link

(2016). Supercontinent and Superplate?. Poster from NAC14.

Poster

(2015). Extending the Cantabrian Orocline to two continents (Gondwana and Laurussia). Paleomagnetism from South Ireland. . EPSL, 432, pp.223-231.

PDF DOI Custom Link

(2015). One or two oroclines in the Variscan orogen of Iberia? Implications for Pangea amalgamation. Geology 43-6, 527-530.

PDF DOI Custom Link

(2015). Significance of detrital zircons in Siluro-Devonian rocks from Iberia. Journal of the Geological Society, 172, 309-322.

PDF DOI Custom Link

(2015). Dating of lithospheric buckling: 40Ar/39Ar ages of syn-orocline strike-slip shear zones in northwestern Iberia. Tectonophysics, 643, 44-54..

PDF DOI Custom Link

(2014). Timing and structural evolution in the limb of an orocline: the Pisuerga-Carrión Unit (southern limb of the Cantabrian Orocline, NW Spain). Tectonophysics, 622, 110–121.

PDF LINK

(2014). The Ediacaran-Early Cambrian detrital zircon record of NW Iberia. Possible sources and paleogeographic constraints.. International Journal of Earth Sciences 103, 5, 1335-1357.

PDF LINK

(2014). Provenance variability along the Early Ordovician north Gondwana margin: Paleogeographic and tectonic implications of U-Pb detrital zircon ages from the Armorican Quartzite of the Iberian Variscan belt. GSA Bulletin (2014) 126 (5-6): 702-719.

PDF LINK

(2013). Tectonic evolution of NW Iberia during the Paleozoic inferred from the geochemical record of detrital rocks in the Cantabrian Zone. Lithos, 182–183, 211–228.

PDF LINK

(2013). Provenance analysis of the Paleozoic sequences of the northern Gondwana margin in NW Iberia: passive margin to Variscan collision and orocline development. Gondwana Research 3, 1089-113.

PDF LINK

(2013). Mathematica code for least-squares cone fitting and equal-area stereonet representation. Computers and Geosciences, 54, 203–210.

PDF LINK

(2013). Kinematic constraints on buckling a lithospheric-scale orocline along the northern margin of Gondwana: A geologic synthesis. Tectonophysics 582, 25-49.

PDF LINK

(2013). Evolución geodinámica del Oroclinal Ibero Armoricano. Geología estructural, modlización análoga y geocronología. Serie Nova Terra.

Preprint Link

(2012). Analogue modeling of lithospheric scale orocline buckling: Constraints on the evolution of the Ibero Armorican Arc.. GSA Bulletin 124, 7-8, 1293-1309.

PDF LINK

(2012). Conical folding in the core of an orocline. A geometric analysis from the Cantabrian Arc (Variscan Belt of NW Iberia).. Journal of Structural Geology. v. 39, 210-223.

PDF LINK

(2012). Buckling an orogen: The Cantabrian Orocline.. GSA Today. v.22, no. 7, 4-7.

PDF LINK

(2012). A virtual tour of the Ibero-Armorican orocline.. Journal of the Virtual Explorer v. 43, paper 2.

PDF LINK

(2011). Modelización análoga del desprendimiento de una raíz litosférica. ¿Puede un oroclinal producir el desprendimiento del manto litosférico?/Analogue modeling of detachment of a lithospheric root. Do oroclines trigger lithospheric detachment?. Geogaceta, 52, 123-126.

PDF Link

(2011). Iberian late-Variscan granitoids: Some considerations on crustal sources and the significance of mantle extraction ages. Lithos, 123, 1-4, 121-132.

PDF DOI Link

(2011). Diachronous post‐orogenic magmatism within a developing orocline in Iberia, European Variscides. Tectonics, 30, TC5008.

PDF DOI Link

(2011). Orocline timing through joint analysis: Insights from the Ibero-Armorican Arc.. Tectonophysics 507, 31–46.

PDF LINK

(2009). Factors affecting finite strain estimation in low-grade, low-strain clastic rocks.. Journal of Structural Geology 31(12) pp. 1586-1596.

PDF LINK

(2008). Determinación de la deformación finita en dos secciones distintas (Talas Ala Tau, Kirguistán y Zona Cantábrica, NO de España). Relaciones entre litología y deformación interna. Stud. Geol. Salman., 44 (2), p 221-258.

PDF LINK

(0001). .