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) en Partial crustal melting beneath the Betic Cordillera (SE Spain): The case study of Mar Menor volcanic suite
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| 92 | "notes": "The Neogene Volcanic Province (NVP) within the Betic | 102 | "notes": "The Neogene Volcanic Province (NVP) within the Betic | ||
| 93 | Cordillera (SE Spain) consists of three main metapelitic enclave | 103 | Cordillera (SE Spain) consists of three main metapelitic enclave | ||
| 94 | suites (from SW to NE: El Hoyazo, Mazarr\u00f3n and Mar Menor). Since | 104 | suites (from SW to NE: El Hoyazo, Mazarr\u00f3n and Mar Menor). Since | ||
| 95 | the NVP represents a singular place in the world where crustal | 105 | the NVP represents a singular place in the world where crustal | ||
| 96 | enclaves were immediately quenched after melting, their | 106 | enclaves were immediately quenched after melting, their | ||
| 97 | microstructures provide a \u201cphotograph\u201d of the conditions at | 107 | microstructures provide a \u201cphotograph\u201d of the conditions at | ||
| 98 | depth just after the moment of the melting. The thermobarometric | 108 | depth just after the moment of the melting. The thermobarometric | ||
| 99 | information provided by the different microstructural assemblages has | 109 | information provided by the different microstructural assemblages has | ||
| 100 | been integrated with the geophysical and geodynamical published data | 110 | been integrated with the geophysical and geodynamical published data | ||
| 101 | into a model of the petrologic evolution of the Mar Menor enclaves. | 111 | into a model of the petrologic evolution of the Mar Menor enclaves. | ||
| 102 | They were equilibrated at 2\u20133 kbar, 850\u2013900 \u00b0C, and | 112 | They were equilibrated at 2\u20133 kbar, 850\u2013900 \u00b0C, and | ||
| 103 | followed a sequence of heating melt producing reactions. A local | 113 | followed a sequence of heating melt producing reactions. A local | ||
| 104 | cooling event evidenced by minor melt crystallization preceded the | 114 | cooling event evidenced by minor melt crystallization preceded the | ||
| 105 | eruption. The lower crustal studies presented in this work contribute | 115 | eruption. The lower crustal studies presented in this work contribute | ||
| 106 | to the knowledge of: (i) the partial melting event beneath the Mar | 116 | to the knowledge of: (i) the partial melting event beneath the Mar | ||
| 107 | Menor volcanic suite through a petrologic detailed study of the | 117 | Menor volcanic suite through a petrologic detailed study of the | ||
| 108 | enclaves; (ii) how the microstructures of fast cooled anatectic rocks | 118 | enclaves; (ii) how the microstructures of fast cooled anatectic rocks | ||
| 109 | play an important role in tracing the magma evolution in a chamber up | 119 | play an important role in tracing the magma evolution in a chamber up | ||
| 110 | to the eruption, and how they can be used as pseudothermobarometers; | 120 | to the eruption, and how they can be used as pseudothermobarometers; | ||
| 111 | (iii) the past and current evolution of the Albor\u00e1n Domain (Betic | 121 | (iii) the past and current evolution of the Albor\u00e1n Domain (Betic | ||
| 112 | Cordillera) and Mediterranean Sea, and how the base of a metapelitic | 122 | Cordillera) and Mediterranean Sea, and how the base of a metapelitic | ||
| 113 | crust has melted within an active geodynamic setting. \u00a9 2007 | 123 | crust has melted within an active geodynamic setting. \u00a9 2007 | ||
| 114 | Elsevier B.V. All rights reserved.", | 124 | Elsevier B.V. All rights reserved.", | ||
| 115 | "notes_translated": { | 125 | "notes_translated": { | ||
| 116 | "es": "The Neogene Volcanic Province (NVP) within the Betic | 126 | "es": "The Neogene Volcanic Province (NVP) within the Betic | ||
| 117 | Cordillera (SE Spain) consists of three main metapelitic enclave | 127 | Cordillera (SE Spain) consists of three main metapelitic enclave | ||
| 118 | suites (from SW to NE: El Hoyazo, Mazarr\u00f3n and Mar Menor). Since | 128 | suites (from SW to NE: El Hoyazo, Mazarr\u00f3n and Mar Menor). Since | ||
| 119 | the NVP represents a singular place in the world where crustal | 129 | the NVP represents a singular place in the world where crustal | ||
| 120 | enclaves were immediately quenched after melting, their | 130 | enclaves were immediately quenched after melting, their | ||
| 121 | microstructures provide a \u201cphotograph\u201d of the conditions at | 131 | microstructures provide a \u201cphotograph\u201d of the conditions at | ||
| 122 | depth just after the moment of the melting. The thermobarometric | 132 | depth just after the moment of the melting. The thermobarometric | ||
| 123 | information provided by the different microstructural assemblages has | 133 | information provided by the different microstructural assemblages has | ||
| 124 | been integrated with the geophysical and geodynamical published data | 134 | been integrated with the geophysical and geodynamical published data | ||
| 125 | into a model of the petrologic evolution of the Mar Menor enclaves. | 135 | into a model of the petrologic evolution of the Mar Menor enclaves. | ||
| 126 | They were equilibrated at 2\u20133 kbar, 850\u2013900 \u00b0C, and | 136 | They were equilibrated at 2\u20133 kbar, 850\u2013900 \u00b0C, and | ||
| 127 | followed a sequence of heating melt producing reactions. A local | 137 | followed a sequence of heating melt producing reactions. A local | ||
| 128 | cooling event evidenced by minor melt crystallization preceded the | 138 | cooling event evidenced by minor melt crystallization preceded the | ||
| 129 | eruption. The lower crustal studies presented in this work contribute | 139 | eruption. The lower crustal studies presented in this work contribute | ||
| 130 | to the knowledge of: (i) the partial melting event beneath the Mar | 140 | to the knowledge of: (i) the partial melting event beneath the Mar | ||
| 131 | Menor volcanic suite through a petrologic detailed study of the | 141 | Menor volcanic suite through a petrologic detailed study of the | ||
| 132 | enclaves; (ii) how the microstructures of fast cooled anatectic rocks | 142 | enclaves; (ii) how the microstructures of fast cooled anatectic rocks | ||
| 133 | play an important role in tracing the magma evolution in a chamber up | 143 | play an important role in tracing the magma evolution in a chamber up | ||
| 134 | to the eruption, and how they can be used as pseudothermobarometers; | 144 | to the eruption, and how they can be used as pseudothermobarometers; | ||
| 135 | (iii) the past and current evolution of the Albor\u00e1n Domain (Betic | 145 | (iii) the past and current evolution of the Albor\u00e1n Domain (Betic | ||
| 136 | Cordillera) and Mediterranean Sea, and how the base of a metapelitic | 146 | Cordillera) and Mediterranean Sea, and how the base of a metapelitic | ||
| 137 | crust has melted within an active geodynamic setting. \u00a9 2007 | 147 | crust has melted within an active geodynamic setting. \u00a9 2007 | ||
| 138 | Elsevier B.V. All rights reserved." | 148 | Elsevier B.V. All rights reserved." | ||
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| 299 | ], | 309 | ], | ||
| 300 | "title": "Partial crustal melting beneath the Betic Cordillera (SE | 310 | "title": "Partial crustal melting beneath the Betic Cordillera (SE | ||
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| 303 | "es": "Partial crustal melting beneath the Betic Cordillera (SE | 313 | "es": "Partial crustal melting beneath the Betic Cordillera (SE | ||
| 304 | Spain): The case study of Mar Menor volcanic suite" | 314 | Spain): The case study of Mar Menor volcanic suite" | ||
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| 308 | "type": "dataset", | 318 | "type": "dataset", | ||
| 309 | "url": | 319 | "url": | ||
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| 313 | } | 323 | } | ||
| 314 | } | 324 | } |