UGR-CSIC, Andalusian Earth Sciences Institute
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Gravity data were obtained during the INCRISIS cruise to address the recent and active near-surface tectonic deformations related to the 2016–2017 seismic sequence within the greater context of the 1993–1994 and 2004 sequences in the central Alboran Sea. This study provided insights into the propagation of recent fault zones and how they are linked to seafloor deformations in addition to their relationships with the former Al Idrisi Fault.
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Multibeam bathymetry to study the morphostructure of the Alboran Sea- ALBA cruise
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Multibeam imagery was collected with a Elac Seabeam 1185 echo sounder in March 2010. This multibeamecho sounder has beams as narrow as 1,5 x 1,5 degrees and a swathwidth in excess of 150 degrees. The data were corrected for heading, depth, pitch, heave, and roll with a redundant Meridian TSS/MAHRS system and with the Port Motril tidal gauge records.
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Scientific objectives from Subproject REN2001-3868-CO3-01 address tectonic-related processes leading to crustal deformation and basin architecture, active tectonics and faulting, deep to shallow seismicity, present-day plate kinematics, and related subsurface structures and seafloor morphology.
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This dataset addresses tectonic-related processes leading to crustal deformation and basin architecture, active tectonics and faulting, deep to shallow seismicity, present-day plate kinematics, and related seafloor morphology.
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Faults related to the tectonic indentation along the Eurasian-African plate boundary in the central Alboran Sea