10 pagesThe Western Medi terranean differs considerably from the Eastern Medi terranean. This is due to the absence of modern active margins in the Western Mediterranean. Instead, there are separate basins underlain by oceanic or thinned continental crust, young in age. The Valencia Trough, the western part of the East-Balearic Sea, as well as the Alboran Sea are examples of such basins. These are the basins where the study areas are located. Insight about the geological structure of the Earth's crust in the study areas is obtained from the geological data from the adjacent land, marine drilling results, but mainly from geophysical dat
Major tectonic units of Spain have been investigated by deep seismic sounding experiments since 1974...
Although the deep structure of the western Mediterranean has been extensively studied (i.e. global t...
16 pages, 10 figuresThe 400 km long Valencia Channel occupies the axis of the Valencia Trough in the...
Seismic refraction and reflection, gravity and well data have been used to constrain the structure a...
The western Mediterranean is the younger part of the Mediterranean, being a basin formed during the ...
The Valencia Trough is an extensional basin that began rifting during the late Oligocene-early Mioce...
First results are presented of a recent onshore seismic survey complementary to the Valsis-2 Cruise,...
European Geosciences Union General Assembly 2017, 23-28 April 2017, Vienna, Austria.-- 1 pageThe wes...
Deep seismic profiling and gravity data show that the continental crust under the Valencia trough ha...
The bathymetry, magnetic anomalies, gravity anomalies and sediment layer is presented to support a y...
The Western Mediterranean realm is characterized by a series of structural arcs that separate contra...
We present a multidisciplinary study of morphology, stratigraphy, sedimentology, tectonic structure,...
19 pagesThe area of study is located at the junction between two of the major turbiditic systems of ...
none3The Mediterranean we presently see is the result of a long geological history of rifting, sprea...
The western Mediterranean is the younger part of the Mediterranean, being a basin formed from late O...
Major tectonic units of Spain have been investigated by deep seismic sounding experiments since 1974...
Although the deep structure of the western Mediterranean has been extensively studied (i.e. global t...
16 pages, 10 figuresThe 400 km long Valencia Channel occupies the axis of the Valencia Trough in the...
Seismic refraction and reflection, gravity and well data have been used to constrain the structure a...
The western Mediterranean is the younger part of the Mediterranean, being a basin formed during the ...
The Valencia Trough is an extensional basin that began rifting during the late Oligocene-early Mioce...
First results are presented of a recent onshore seismic survey complementary to the Valsis-2 Cruise,...
European Geosciences Union General Assembly 2017, 23-28 April 2017, Vienna, Austria.-- 1 pageThe wes...
Deep seismic profiling and gravity data show that the continental crust under the Valencia trough ha...
The bathymetry, magnetic anomalies, gravity anomalies and sediment layer is presented to support a y...
The Western Mediterranean realm is characterized by a series of structural arcs that separate contra...
We present a multidisciplinary study of morphology, stratigraphy, sedimentology, tectonic structure,...
19 pagesThe area of study is located at the junction between two of the major turbiditic systems of ...
none3The Mediterranean we presently see is the result of a long geological history of rifting, sprea...
The western Mediterranean is the younger part of the Mediterranean, being a basin formed from late O...
Major tectonic units of Spain have been investigated by deep seismic sounding experiments since 1974...
Although the deep structure of the western Mediterranean has been extensively studied (i.e. global t...
16 pages, 10 figuresThe 400 km long Valencia Channel occupies the axis of the Valencia Trough in the...