A new geodynamic model of the Azores archipelago: preliminary results
Authors: Almeida Jaime , Duarte João , Rosas Filipe , Fernandes Rui , Geraldes Fernando , Carvalho Luis , Ramalho Ricardo 
Published: March 2024

The Azores archipelago is an integral part of the Macaronesian geographic region (which also includes the volcanic archipelagos of Madeira, Selvagens, Canaries and Cape Verde). This region, located in the centre of Atlantic Ocean, has its individual islands spread around a triple junction, which has been suggested to affected by a plume-ridge interaction (Storch et al., 2020; Beier et al., 2022). One of the major questions surrounding its history concern the why/how the Terceira Rift (i.e., the NW-SE oriented connection between the mid-ocean ridge and the Gloria Fault Zone) was formed.To explore this issue, we have run sets of 3D viscoelastoplastic models for the region using the state-of-the-art modelling code LaMEM (Kaus et al., 2016). As our objective was to evaluate how the geological data and the suggested evolution for the region fit geodynamic constraints. We based our numerical models on previously established evolutionary models for the region, such as the leaky transform model (Madeira and Ribeiro, 1990).Preliminary results hint that the formation of the Terceira Rift could be formed as the result of a shift in the regional tectonic forcing, which we attribute to the collision between the Iberian and Eurasian plates. Furthermore, our results suggest that a strong rheological contrast in the region was required to ensure the localization of deformation. Models without this feature tended to maintain a simple E-W connection between the Gloria Fault Zone and the southern part of the mid-ocean ridge.This work was funded by the Portuguese Funda&#231;&#227;o para a Ci&#234;ncia e a Tecnologia (FCT) I.P./MCTES through projects GEMMA (https://doi.org/10.54499/PTDC/CTA-GEO/2083/2021) and national funds (PIDDAC) &#8211; UIDB/50019/2020 (https://doi.org/10.54499/UIDB/50019/2020), UIDP/50019/2020 (https://doi.org/10.54499/UIDP/50019/2020) and LA/P/0068/2020 (https://doi.org/10.54499/LA/P/0068/2020).&#160;ReferencesBeier, C. et al. (2022) &#8216;The submarine Azores Plateau: Evidence for a waning mantle plume?&#8217;, Marine Geology, 451, p. 106858. Available at: https://doi.org/10.1016/j.margeo.2022.106858.Kaus, B.J.P. et al. (2016) &#8216;Forward and Inverse Modelling of Lithospheric Deformation on Geological Timescales&#8217;, NIC Series, 48, pp. 978&#8211;3.Luis, J.F. and Miranda, J.M. (2008) &#8216;Reevaluation of magnetic chrons in the North Atlantic between 35&#176;N and 47&#176;N: Implications for the formation of the Azores Triple Junction and associated plateau&#8217;, Journal of Geophysical Research: Solid Earth, 113(B10). Available at: https://doi.org/10.1029/2007JB005573.Madeira, J. and Ribeiro, A. (1990) &#8216;Geodynamic models for the Azores triple junction: A contribution from tectonics&#8217;, Tectonophysics, 184(3&#8211;4), pp. 405&#8211;415. Available at: https://doi.org/10.1016/0040-1951(90)90452-E.Storch, B. et al. (2020) &#8216;Rifting of the oceanic Azores Plateau with episodic volcanic activity&#8217;, Scientific Reports, 10(1), p. 19718. Available at: https://doi.org/10.1038/s41598-020-76691-1.