Metadata 1678
Offshore seismic lines from Croatia
Since 1981 approximately 35 900 km of seismic lines were acquired, covering nearly all of Estonian offshore area on different grid, with the exception of the shallow nearshore areas. The seismic profiles are available in analogue or in digital format. Present digital seismic data is available in Meridata file format.
Sub-bottom profile data shows the rock features and the sediment layers that are below the seabed.A sub bottom profile is created by sending sound or seismic waves from a boat to the seabed. The length of time it takes for these waves to return from the seabed to the boat is measured. The length of time tells us how hard the material below the seabed is. Hard material such as solid rock returns the sound wave very quickly. Soft material such as mud returns the sound wave very slowly. This allows us to buil...
Geophysical data for which GEUS (Geological Survey of Denmark and Greenland) is custodian
Offshore seismic and multibeam data collected by Istanbul University,Institute of Marine Sciences and Management
Offshore high resolution seismic lines on recovered from the shelf and basins of the Sea of Marmara, which provide stratigraphic relations of the late Quaternary deposits, and tectonic setting related to North Anatolian Fault segments.
From 1976 to 1991, approximately 24,500 km of Common Depth Point (CDP) seismic lines were acquired, covering nearly all of Latvia's offshore area on a 2x2 km seismic grid, with the exception of the shallowest nearshore areas. The seismic profiles are available in analogue format on magnetic tapes, with some of them having been processed and available digitally in *.sgy file format.
Geophysical data from Malta. Due to confidentiality data are shown as polygons
Offshore seismic lines were acquired by Prichornomor State Regional Geological Enterprise (PrichornomorSRGE) during geological surveys at a scale of 1:200,000 in 2007–2011.
Offshore seismic lines were acquired by Prichornomor State Regional Geological Enterprise (PrichornomorSRGE) during geological surveys at a scale of 1:200,000 in 2007–2011.