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.

This data and documents are part of a DVD prepared by Dr. John K. Hall the former Vice Chairman of the IBCM (International Bathymetric Chart of the Mediterranean) containing some scanned charts, raster cartography and scientific papers related to the bathymetry, magnetics, gravity, Plio-Quaternary sediments, Seismicity, and Bottom Sediment maps of the Mediterranean Sea with their explanatory notes. The charts have been prepared mainly in collaboration with OGS, University of Trieste, Institute for Geophysics in Hamburg, the Russian Academy of Science and the Russian Federation under the authority of IOC.

The content of the file package comprises: 1) Postcards in pdf format, regarding the Mediterranean Sea, showing a Tectonic Map, a Marine Magnetic a Anomalies Map, a Sediment Map, a Plio-Quaternary Map, a Seismicity Map and a Bouger Gravity Anomalies Map (see directory wetransfer-253deb); 2) Books: GEOLOGICAL FRAMEWORK of the LEVANT VOLUME I: CYPRUS and SYRIA and VOLUME II: The LEVANTINE BASIN and ISRAEL ( see directory wetransfer-253deb); 3) Digital bathymetric contour and coastline data from the First Edition of the International Bathymetric Chart of the Mediterranean (IBCM) (see directory wetransfer-c507a2);

This data and documents are part of a DVD prepared by Dr. John K. Hall the former Vice Chairman of the IBCM (International Bathymetric Chart of the Mediterranean) containing some scanned charts, raster cartography and scientific papers related to the bathymetry, magnetics, gravity, Plio-Quaternary sediments, Seismicity, and Bottom Sediment maps of the Mediterranean Sea with their explanatory notes. The charts have been prepared mainly in collaboration with OGS, University of Trieste, Institute for Geophysics in Hamburg, the Russian Academy of Science and the Russian Federation under the authority of IOC.

This data and documents are part of a DVD prepared by Dr. John K. Hall the former Vice Chairman of the IBCM (International Bathymetric Chart of the Mediterranean) contain the scanned charts and scientific papers related to the bathymetry, magnetics, gravity, Plio-Quaternary sediments, Seismicity, and Bottom Sediment maps of the Mediterranean Sea with their explanatory notes. The charts have been prepared in collaboration mainly with OGS, University of Trieste, Institute for Geophysics in Hamburg, the Russian Academy of Science and the Russian Federation under the authority of IOC.

This data and documets are part of a DVD prepared by Dr. John K. Hall the former Vice Chairman of the IBCM (International Bathymetric Chart of the Mediterranean) contain the scanned charts and scientific papers related to the bathymetry, magnetics, gravity, Plio-Quaternary sediments, Seismicity, and Bottom Sediment maps of the Mediterranean Sea with their explanatory notes. The charts have been prepared in collaboration mainly with OGS, University of Trieste, Institute for Geophysics in Hamburg, the Russian Academy of Science and the Russian Federation under the authority of IOC.

This data is part of a DVD prepared by Dr. John K. Hall the former Vice Chairman of the IBCM (International Bathymetric Chart of the Mediterranean) with all the scanned charts and scientific papers related to the bathymetry, magnetics, gravity, Plio-Quaternary sediments, Seismicity, and Bottom Sediment maps of the Mediterranean Sea with their explanatory notes. The charts have been prepared in collaboration mainly with OGS, University of Trieste, Institute for Geophysics in Hamburg, the Russian Academy of Science, the Russian Federation under the authority of IOC. The huge amount of data doesn’t allow to upload all the files together and so the data will be split at least into 4 parts.