SUBSIDENCE HISTORY, CRUSTAL STRUCTURE, AND THERMAL EVOLUTION OF THE VALENCIA TROUGH - A YOUNG EXTENSIONAL BASIN IN THE WESTERN MEDITERRANEAN
The Valencia Trough is an extensional basin that began rifting during the late Oligocene-early Miocene, yet is is located within a region of compression between the European and African plates. Although the trough appears symmetric on bathymetric maps, seismic and gravity and geoid data indicate a f...
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| Médium: | Journal article |
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1992
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