2003
DOI: 10.1016/s0169-555x(02)00168-x
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The Balearic Promontory geomorphology (western Mediterranean): morphostructure and active processes

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Cited by 101 publications
(63 citation statements)
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“…This weak activity is the likely reason for the scarcity of studies of the active tectonics (Silva et al, 1997(Silva et al, , 1999(Silva et al, , 2000(Silva et al, , 2001Giménez and Gelabert, 2002;Giménez, 2003;Gelabert et al, 2005). Other onshore studies have described the Plio-Quaternary activity in the Balearic Promontory (Roca, 1996;Acosta et al, 2001Acosta et al, , 2002Acosta et al, , 2004Maillard and Mauffret, 2013).…”
Section: Introductionmentioning
confidence: 94%
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“…This weak activity is the likely reason for the scarcity of studies of the active tectonics (Silva et al, 1997(Silva et al, , 1999(Silva et al, , 2000(Silva et al, , 2001Giménez and Gelabert, 2002;Giménez, 2003;Gelabert et al, 2005). Other onshore studies have described the Plio-Quaternary activity in the Balearic Promontory (Roca, 1996;Acosta et al, 2001Acosta et al, , 2002Acosta et al, , 2004Maillard and Mauffret, 2013).…”
Section: Introductionmentioning
confidence: 94%
“…Several investigations (Roca, 1996;Acosta et al, 2001Acosta et al, , 2002Acosta et al, and 2004Maillard and Mauffret, 2013) describe NE-SW and NW-SE normal and strike-slip faults affecting the Plio-Quaternary materials in the offshore area of the Balearic Islands.…”
Section: Geodynamic Settingmentioning
confidence: 99%
“…1) what is geomorphologically known as the Balearic Promontory, one of the main morphostructural features of the western Mediterranean Basin (Acosta et al 2002). The Promontory represents a sort of carbonate counterpart to the terrigenous-dominated margins of the Mediterranean Iberian Peninsula.…”
Section: Geomorphologymentioning
confidence: 99%
“…The sampling sites were located over 200 and 900 m depth (shelf break and middle slope, respectively) and present different environmental conditions (Pinot et al 2002;López-Jurado et al 2008). At the southern station of Mallorca, the upper slope is irregular, with numerous small canyons, while it is smooth in the northern station (Acosta et al 2002). Two additional polychelid zoeal stages were captured between 300 and 400 m depth over the slope of Blanes canyon (NW Mediterranean) during 2004 under the ''Observation, analysis and modelling of the Mediterranenan Sea'' (OAMMS-04) survey, and were also used for photographic record.…”
Section: Samplingmentioning
confidence: 99%