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En el instante 23 de junio de 2026, 15:59:44 UTC,
-
Modificado el valor del campo
spatial_coverage
a[{'bbox': '{"type": "Polygon", "coordinates": [[[-2.34, 37.38], [-0.69, 37.38], [-0.69, 38.76], [-2.34, 38.76], [-2.34, 37.38]]]}', 'centroid': '{"type": "Point", "coordinates": [-1.515, 38.07]}', 'text': 'Región de Murcia', 'uri': 'http://datos.gob.es/recurso/sector-publico/territorio/Autonomia/Region-Murcia'}]
en The morpho-tectonic setting of the Southeast margin of Iberia and the adjacent oceanic Algero-Balearic Basin
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| 92 | "notes": "Multi-beam bathymetry and high-resolution low-penetration | 92 | "notes": "Multi-beam bathymetry and high-resolution low-penetration | ||
| 93 | seismic reflection profiles of the offshore extensions of the Betic | 93 | seismic reflection profiles of the offshore extensions of the Betic | ||
| 94 | Internal Zone off Sierra de Cartagena-La Union margin along its south | 94 | Internal Zone off Sierra de Cartagena-La Union margin along its south | ||
| 95 | side and the Mar Menor margin along its east side, the Mazarron | 95 | side and the Mar Menor margin along its east side, the Mazarron | ||
| 96 | Escarpment forming its southern boundary and the adjacent oceanic | 96 | Escarpment forming its southern boundary and the adjacent oceanic | ||
| 97 | Algero-Balearic basin have provided images of the neo-tectonic | 97 | Algero-Balearic basin have provided images of the neo-tectonic | ||
| 98 | structures of the region equal to those provided by subaerial | 98 | structures of the region equal to those provided by subaerial | ||
| 99 | photography. For the first time we mapped with unprecedented detail | 99 | photography. For the first time we mapped with unprecedented detail | ||
| 100 | the Mazarron Escarpment and the Southeast margin of Iberia.The | 100 | the Mazarron Escarpment and the Southeast margin of Iberia.The | ||
| 101 | first-order structures of the region are due to the consequence of the | 101 | first-order structures of the region are due to the consequence of the | ||
| 102 | collision of the African and Eurasian plates during the Alpine orogeny | 102 | collision of the African and Eurasian plates during the Alpine orogeny | ||
| 103 | in late Oligocene-Middle Miocene, the westward migration of the | 103 | in late Oligocene-Middle Miocene, the westward migration of the | ||
| 104 | Alboran plate in the Middle Miocene and the desiccation of the | 104 | Alboran plate in the Middle Miocene and the desiccation of the | ||
| 105 | Mediterranean in the Messinian (Late Miocene) that led to the | 105 | Mediterranean in the Messinian (Late Miocene) that led to the | ||
| 106 | deposition of evaporites in the Algero-Balearic basin and erosion of | 106 | deposition of evaporites in the Algero-Balearic basin and erosion of | ||
| 107 | the Mazarron Escarpment, the Sierra de Cartagena-La Union shelf, the | 107 | the Mazarron Escarpment, the Sierra de Cartagena-La Union shelf, the | ||
| 108 | Mar Menor margin and the adjacent coast. Our data images second order | 108 | Mar Menor margin and the adjacent coast. Our data images second order | ||
| 109 | tectonic features (neo-tectonic features) superimposed on the larger | 109 | tectonic features (neo-tectonic features) superimposed on the larger | ||
| 110 | structures. These include the deformation of the strata in the | 110 | structures. These include the deformation of the strata in the | ||
| 111 | Algero-Balearic basin by the gliding of the Plio-Quaternary sediments | 111 | Algero-Balearic basin by the gliding of the Plio-Quaternary sediments | ||
| 112 | on Messinian halite on the margins of the basin and sediment loading | 112 | on Messinian halite on the margins of the basin and sediment loading | ||
| 113 | in its center, the Late Miocene-Quaternary deformation of the area | 113 | in its center, the Late Miocene-Quaternary deformation of the area | ||
| 114 | north of the Mazarron Escarpment resulting from the continuous oblique | 114 | north of the Mazarron Escarpment resulting from the continuous oblique | ||
| 115 | convergence of the African and Eurasian plates in a NNW-SSE direction, | 115 | convergence of the African and Eurasian plates in a NNW-SSE direction, | ||
| 116 | the Miocene to Pleistocene volcanic edifices and pinnacles (dikes), | 116 | the Miocene to Pleistocene volcanic edifices and pinnacles (dikes), | ||
| 117 | the pockmarks formed by the extrusion of gas/water via faults and the | 117 | the pockmarks formed by the extrusion of gas/water via faults and the | ||
| 118 | massive gravitational failure of the Mazarron Escarpment triggered by | 118 | massive gravitational failure of the Mazarron Escarpment triggered by | ||
| 119 | this plate convergence. The data also show in detail features formed | 119 | this plate convergence. The data also show in detail features formed | ||
| 120 | on the Mazarron Escarpment during the Messinian, Pliocene and | 120 | on the Mazarron Escarpment during the Messinian, Pliocene and | ||
| 121 | Pleistocene regressions and those on the shelf formed during the | 121 | Pleistocene regressions and those on the shelf formed during the | ||
| 122 | Pleistocene glacially induced regressions/transgression and sediment | 122 | Pleistocene glacially induced regressions/transgression and sediment | ||
| 123 | drifts generated by modern currents.", | 123 | drifts generated by modern currents.", | ||
| 124 | "notes_translated": { | 124 | "notes_translated": { | ||
| 125 | "es": "Multi-beam bathymetry and high-resolution low-penetration | 125 | "es": "Multi-beam bathymetry and high-resolution low-penetration | ||
| 126 | seismic reflection profiles of the offshore extensions of the Betic | 126 | seismic reflection profiles of the offshore extensions of the Betic | ||
| 127 | Internal Zone off Sierra de Cartagena-La Union margin along its south | 127 | Internal Zone off Sierra de Cartagena-La Union margin along its south | ||
| 128 | side and the Mar Menor margin along its east side, the Mazarron | 128 | side and the Mar Menor margin along its east side, the Mazarron | ||
| 129 | Escarpment forming its southern boundary and the adjacent oceanic | 129 | Escarpment forming its southern boundary and the adjacent oceanic | ||
| 130 | Algero-Balearic basin have provided images of the neo-tectonic | 130 | Algero-Balearic basin have provided images of the neo-tectonic | ||
| 131 | structures of the region equal to those provided by subaerial | 131 | structures of the region equal to those provided by subaerial | ||
| 132 | photography. For the first time we mapped with unprecedented detail | 132 | photography. For the first time we mapped with unprecedented detail | ||
| 133 | the Mazarron Escarpment and the Southeast margin of Iberia.The | 133 | the Mazarron Escarpment and the Southeast margin of Iberia.The | ||
| 134 | first-order structures of the region are due to the consequence of the | 134 | first-order structures of the region are due to the consequence of the | ||
| 135 | collision of the African and Eurasian plates during the Alpine orogeny | 135 | collision of the African and Eurasian plates during the Alpine orogeny | ||
| 136 | in late Oligocene-Middle Miocene, the westward migration of the | 136 | in late Oligocene-Middle Miocene, the westward migration of the | ||
| 137 | Alboran plate in the Middle Miocene and the desiccation of the | 137 | Alboran plate in the Middle Miocene and the desiccation of the | ||
| 138 | Mediterranean in the Messinian (Late Miocene) that led to the | 138 | Mediterranean in the Messinian (Late Miocene) that led to the | ||
| 139 | deposition of evaporites in the Algero-Balearic basin and erosion of | 139 | deposition of evaporites in the Algero-Balearic basin and erosion of | ||
| 140 | the Mazarron Escarpment, the Sierra de Cartagena-La Union shelf, the | 140 | the Mazarron Escarpment, the Sierra de Cartagena-La Union shelf, the | ||
| 141 | Mar Menor margin and the adjacent coast. Our data images second order | 141 | Mar Menor margin and the adjacent coast. Our data images second order | ||
| 142 | tectonic features (neo-tectonic features) superimposed on the larger | 142 | tectonic features (neo-tectonic features) superimposed on the larger | ||
| 143 | structures. These include the deformation of the strata in the | 143 | structures. These include the deformation of the strata in the | ||
| 144 | Algero-Balearic basin by the gliding of the Plio-Quaternary sediments | 144 | Algero-Balearic basin by the gliding of the Plio-Quaternary sediments | ||
| 145 | on Messinian halite on the margins of the basin and sediment loading | 145 | on Messinian halite on the margins of the basin and sediment loading | ||
| 146 | in its center, the Late Miocene-Quaternary deformation of the area | 146 | in its center, the Late Miocene-Quaternary deformation of the area | ||
| 147 | north of the Mazarron Escarpment resulting from the continuous oblique | 147 | north of the Mazarron Escarpment resulting from the continuous oblique | ||
| 148 | convergence of the African and Eurasian plates in a NNW-SSE direction, | 148 | convergence of the African and Eurasian plates in a NNW-SSE direction, | ||
| 149 | the Miocene to Pleistocene volcanic edifices and pinnacles (dikes), | 149 | the Miocene to Pleistocene volcanic edifices and pinnacles (dikes), | ||
| 150 | the pockmarks formed by the extrusion of gas/water via faults and the | 150 | the pockmarks formed by the extrusion of gas/water via faults and the | ||
| 151 | massive gravitational failure of the Mazarron Escarpment triggered by | 151 | massive gravitational failure of the Mazarron Escarpment triggered by | ||
| 152 | this plate convergence. The data also show in detail features formed | 152 | this plate convergence. The data also show in detail features formed | ||
| 153 | on the Mazarron Escarpment during the Messinian, Pliocene and | 153 | on the Mazarron Escarpment during the Messinian, Pliocene and | ||
| 154 | Pleistocene regressions and those on the shelf formed during the | 154 | Pleistocene regressions and those on the shelf formed during the | ||
| 155 | Pleistocene glacially induced regressions/transgression and sediment | 155 | Pleistocene glacially induced regressions/transgression and sediment | ||
| 156 | drifts generated by modern currents." | 156 | drifts generated by modern currents." | ||
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