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Submerged coastal notches characterize the coast of the wider Rijeka area, NW Croatian coast, Adriatic Sea. These notches originate from a notch formed approximately 2,000years ago, their depth ranges between 0.50 and 1.15m and their subsidence history is a matter of debate. A detailed study of all the available data in relation to the tectonics of the area was made using signal analysis techniques...
The geodetic inversion technique was used to model the fault pattern responsible for the uplifted Holocene notches along the NE Rhodes Island coast (SE edge of the Hellenic (Aegean) Arc). Input in the modeling was the elevation of uplifted notches, up to 6000 yr old, which are interpreted to reflect remains of fossil shorelines, to testify to a series of earthquakes producing both uplift and subsidence...
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