The Solid Earth dynamics, hazards and resources research group investigates the composition, structure, dynamics, and evolution of the solid Earth, from the deep mantle up to the surface, and with implications for resources and hazards. Our research gives a particular emphasis on the processes that shape ocean island volcanoes, continents and orogenic belts, and continental margins. Our goal is to provide a solid knowledge foundation to better tackle critical challenges such as those posed by:  Earthquakes and volcanism, with research covering from the fundamental investigation of seismogenesis and volcanogenesis to the development of innovative monitoring techniques;  Mineral and hydrocarbon resources, from understanding their genesis to develop their sustainable exploration and exploitation;  Global and climate change, using the geological past as the key to the understand present and future trends; and  our scientific understanding of the fundamentals of our planet’s geodynamics, as the knowledge base of all Earth System science. To achieve this, we employ multidisciplinary approaches that combine geological and geophysical field, experimental, laboratorial, and numerical work, solidly anchored in international collaborations. Particular attention is given to the privileged natural laboratory of the Atlantic Region, with its numerous volcanic archipelagos, different types of margin, and challenging continental surroundings.
Scientific Highlights 2017
The role of internal growth processes in ocean island evolution
The growth and decay of ocean-island volcanoes are intrinsically linked to vertical movements. While the causes for subsidence are better understood, uplift mechanisms remain enigmatic. In order to unravel the origins of ocean island uplift, researchers at IDL led an international effort to study Santa Maria (Azores), an island that should be experiencing subsidence but yet is famous for its exposed submarine sequences, which suggest uplift. Using a combination of detailed fieldwork and isotopic geochronology, this work documented changes of relative sea level to reconstruct the vertical movement history of Santa Maria. The results were published in GSA Bulletin (Ramalho et al., 2017), with the paper being highlighted in EOS (AGU’s magazine). The work revealed that Santa Maria exhibits a complex evolutionary history spanning 6 m.y., with significant subsidence followed by uplift equal in magnitude but at a slower rate. This uplift is mostly likely caused by crustal thickening by basal intrusions, suggesting that intrusive processes play a significant role even on islands standing on young lithosphere, such as in the Azores.
Ambient seismic noise tomography integrating seafloor- and land-based data
Ambient noise (AN) surface wave tomography is now a common tool in seismology. But, until recently, it has not been successfully applied in the investigation of margins where land (LS) and Ocean (OBS) seismic stations data must be combined. In the study of Corela et al., 2017, 24 OBS deployed in the Gulf of Cadiz and 7 LS in the South of Portugal were used together to image the sedimentary and crustal structure beneath SW Iberia. The procedure used was straightforward: i) compute AN cross-correlations to obtain empirical Green’s functions between all station pairs; ii) group velocity dispersion analysis; iii) two-step inversion of the dispersion curves to obtain the 3D distribution of the S-wave velocities. Despite the gap between the OBS and LS locations, the derived velocity model displayed a good correlation with the known geological structure, being locally in agreement with the models proposed by other studies using near vertical, refraction and wide- -angle seismic profiling. Results showed that it is possible to integrate seafloor- and land-based stations to perform AN tomography to derive a model of the structure in the transition domain between continent and ocean.