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En el instante 23 de junio de 2026, 16:10:56 UTC,
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Modificado el valor del campo
spatial_coverage
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en Do extrusion ages reflect magma generation processes at depth? An example from the Neogene Volcanic Province of SE Spain
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| 88 | "notes": "The high-K calc-alkaline volcanic rocks along the Neogene | 88 | "notes": "The high-K calc-alkaline volcanic rocks along the Neogene | ||
| 89 | Volcanic Province of SE Spain represent crustal anatectic melts mixed | 89 | Volcanic Province of SE Spain represent crustal anatectic melts mixed | ||
| 90 | with mantle components during the opening of the Alboran Sea. | 90 | with mantle components during the opening of the Alboran Sea. | ||
| 91 | Partially melted metapelitic enclaves, along with the geochemical | 91 | Partially melted metapelitic enclaves, along with the geochemical | ||
| 92 | signature, provide evidence of their crustal source. U-Pb SHRIMP | 92 | signature, provide evidence of their crustal source. U-Pb SHRIMP | ||
| 93 | geochronology on monazite and zircon from enclaves and their hosting | 93 | geochronology on monazite and zircon from enclaves and their hosting | ||
| 94 | lavas in the localities of El Hoyazo, MazarrA(3)n and Mar Menor | 94 | lavas in the localities of El Hoyazo, MazarrA(3)n and Mar Menor | ||
| 95 | reveals variable delays between the melting at depth and the eruption | 95 | reveals variable delays between the melting at depth and the eruption | ||
| 96 | of the volcanics. These data indicate that: (1) the most important | 96 | of the volcanics. These data indicate that: (1) the most important | ||
| 97 | event of anatexis in the Neogene spanned at least the 3 m.y. interval | 97 | event of anatexis in the Neogene spanned at least the 3 m.y. interval | ||
| 98 | between 12 and 9 Ma; (2) there is no trend in age of crustal melting; | 98 | between 12 and 9 Ma; (2) there is no trend in age of crustal melting; | ||
| 99 | and (3) the delay between magma generation and extrusion varies from | 99 | and (3) the delay between magma generation and extrusion varies from | ||
| 100 | more than 3 m.y. at El Hoyazo to similar to 0.5 m.y. and possibly 2.5 | 100 | more than 3 m.y. at El Hoyazo to similar to 0.5 m.y. and possibly 2.5 | ||
| 101 | m.y. at Mar Menor, with no significant delay measurable at | 101 | m.y. at Mar Menor, with no significant delay measurable at | ||
| 102 | MazarrA(3)n. The variable time delay between anatexis and lava | 102 | MazarrA(3)n. The variable time delay between anatexis and lava | ||
| 103 | extrusion indicates that radiometric ages of volcanics may provide | 103 | extrusion indicates that radiometric ages of volcanics may provide | ||
| 104 | misleading information on the timing of magma genesis occurring at | 104 | misleading information on the timing of magma genesis occurring at | ||
| 105 | depth. This highlights the pitfall of basing detailed geodynamic | 105 | depth. This highlights the pitfall of basing detailed geodynamic | ||
| 106 | models on volcanic extrusion ages alone.", | 106 | models on volcanic extrusion ages alone.", | ||
| 107 | "notes_translated": { | 107 | "notes_translated": { | ||
| 108 | "es": "The high-K calc-alkaline volcanic rocks along the Neogene | 108 | "es": "The high-K calc-alkaline volcanic rocks along the Neogene | ||
| 109 | Volcanic Province of SE Spain represent crustal anatectic melts mixed | 109 | Volcanic Province of SE Spain represent crustal anatectic melts mixed | ||
| 110 | with mantle components during the opening of the Alboran Sea. | 110 | with mantle components during the opening of the Alboran Sea. | ||
| 111 | Partially melted metapelitic enclaves, along with the geochemical | 111 | Partially melted metapelitic enclaves, along with the geochemical | ||
| 112 | signature, provide evidence of their crustal source. U-Pb SHRIMP | 112 | signature, provide evidence of their crustal source. U-Pb SHRIMP | ||
| 113 | geochronology on monazite and zircon from enclaves and their hosting | 113 | geochronology on monazite and zircon from enclaves and their hosting | ||
| 114 | lavas in the localities of El Hoyazo, MazarrA(3)n and Mar Menor | 114 | lavas in the localities of El Hoyazo, MazarrA(3)n and Mar Menor | ||
| 115 | reveals variable delays between the melting at depth and the eruption | 115 | reveals variable delays between the melting at depth and the eruption | ||
| 116 | of the volcanics. These data indicate that: (1) the most important | 116 | of the volcanics. These data indicate that: (1) the most important | ||
| 117 | event of anatexis in the Neogene spanned at least the 3 m.y. interval | 117 | event of anatexis in the Neogene spanned at least the 3 m.y. interval | ||
| 118 | between 12 and 9 Ma; (2) there is no trend in age of crustal melting; | 118 | between 12 and 9 Ma; (2) there is no trend in age of crustal melting; | ||
| 119 | and (3) the delay between magma generation and extrusion varies from | 119 | and (3) the delay between magma generation and extrusion varies from | ||
| 120 | more than 3 m.y. at El Hoyazo to similar to 0.5 m.y. and possibly 2.5 | 120 | more than 3 m.y. at El Hoyazo to similar to 0.5 m.y. and possibly 2.5 | ||
| 121 | m.y. at Mar Menor, with no significant delay measurable at | 121 | m.y. at Mar Menor, with no significant delay measurable at | ||
| 122 | MazarrA(3)n. The variable time delay between anatexis and lava | 122 | MazarrA(3)n. The variable time delay between anatexis and lava | ||
| 123 | extrusion indicates that radiometric ages of volcanics may provide | 123 | extrusion indicates that radiometric ages of volcanics may provide | ||
| 124 | misleading information on the timing of magma genesis occurring at | 124 | misleading information on the timing of magma genesis occurring at | ||
| 125 | depth. This highlights the pitfall of basing detailed geodynamic | 125 | depth. This highlights the pitfall of basing detailed geodynamic | ||
| 126 | models on volcanic extrusion ages alone." | 126 | models on volcanic extrusion ages alone." | ||
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| 260 | "uri": | 231 | "uri": | ||
| 261 | ttp://datos.gob.es/recurso/sector-publico/territorio/Pais/Espa\u00f1a" | 232 | ttp://datos.gob.es/recurso/sector-publico/territorio/Pais/Espa\u00f1a" | ||
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| 264 | "spatial_uri": | 235 | "spatial_uri": | ||
| 265 | tp://datos.gob.es/recurso/sector-publico/territorio/Pais/Espa\u00f1a", | 236 | tp://datos.gob.es/recurso/sector-publico/territorio/Pais/Espa\u00f1a", | ||
| 266 | "state": "active", | 237 | "state": "active", | ||
| 267 | "study_variables": { | 238 | "study_variables": { | ||
| 268 | "es": "" | 239 | "es": "" | ||
| 269 | }, | 240 | }, | ||
| 270 | "tag_uri": [ | 241 | "tag_uri": [ | ||
| 271 | 242 | ||||
| 272 | tp://inspire.ec.europa.eu/metadata-codelist/TopicCategory/environment" | 243 | tp://inspire.ec.europa.eu/metadata-codelist/TopicCategory/environment" | ||
| 273 | ], | 244 | ], | ||
| 274 | "tags": [ | 245 | "tags": [ | ||
| 275 | { | 246 | { | ||
| 276 | "display_name": "geologia", | 247 | "display_name": "geologia", | ||
| 277 | "id": "e083ea64-4b42-4adb-bf37-583e01a2a9d9", | 248 | "id": "e083ea64-4b42-4adb-bf37-583e01a2a9d9", | ||
| 278 | "name": "geologia", | 249 | "name": "geologia", | ||
| 279 | "state": "active", | 250 | "state": "active", | ||
| 280 | "vocabulary_id": null | 251 | "vocabulary_id": null | ||
| 281 | }, | 252 | }, | ||
| 282 | { | 253 | { | ||
| 283 | "display_name": "marino", | 254 | "display_name": "marino", | ||
| 284 | "id": "004084d1-68d8-46ca-842a-c10278540bc9", | 255 | "id": "004084d1-68d8-46ca-842a-c10278540bc9", | ||
| 285 | "name": "marino", | 256 | "name": "marino", | ||
| 286 | "state": "active", | 257 | "state": "active", | ||
| 287 | "vocabulary_id": null | 258 | "vocabulary_id": null | ||
| 288 | } | 259 | } | ||
| 289 | ], | 260 | ], | ||
| 290 | "thematic_area": [ | 261 | "thematic_area": [ | ||
| 291 | "espacios_protegidos" | 262 | "espacios_protegidos" | ||
| 292 | ], | 263 | ], | ||
| 293 | "theme_es": [ | 264 | "theme_es": [ | ||
| 294 | "http://datos.gob.es/kos/sector-publico/sector/medio-ambiente" | 265 | "http://datos.gob.es/kos/sector-publico/sector/medio-ambiente" | ||
| 295 | ], | 266 | ], | ||
| 296 | "title": "Do extrusion ages reflect magma generation processes at | 267 | "title": "Do extrusion ages reflect magma generation processes at | ||
| 297 | depth? An example from the Neogene Volcanic Province of SE Spain", | 268 | depth? An example from the Neogene Volcanic Province of SE Spain", | ||
| 298 | "title_translated": { | 269 | "title_translated": { | ||
| 299 | "es": "Do extrusion ages reflect magma generation processes at | 270 | "es": "Do extrusion ages reflect magma generation processes at | ||
| 300 | depth? An example from the Neogene Volcanic Province of SE Spain" | 271 | depth? An example from the Neogene Volcanic Province of SE Spain" | ||
| 301 | }, | 272 | }, | ||
| 302 | "topic": | 273 | "topic": | ||
| 303 | "http://inspire.ec.europa.eu/metadata-codelist/TopicCategory/biota", | 274 | "http://inspire.ec.europa.eu/metadata-codelist/TopicCategory/biota", | ||
| 304 | "type": "dataset", | 275 | "type": "dataset", | ||
| 305 | "url": | 276 | "url": | ||
| 306 | //iepnb.es:443/catalogo/dataset/30bc4ab0-bb9d-52e6-9fda-7f78a9bfab32", | 277 | //iepnb.es:443/catalogo/dataset/30bc4ab0-bb9d-52e6-9fda-7f78a9bfab32", | ||
| 307 | "version_notes": { | 278 | "version_notes": { | ||
| 308 | "es": "" | 279 | "es": "" | ||
| 309 | } | 280 | } | ||
| 310 | } | 281 | } |