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| 88 | "notes": "Crustal xenoliths from the Neogene Volcanic Province (NVP) | 98 | "notes": "Crustal xenoliths from the Neogene Volcanic Province (NVP) | ||
| 89 | of the Betic Cordillera, SE Spain, constitute an unusual suite of | 99 | of the Betic Cordillera, SE Spain, constitute an unusual suite of | ||
| 90 | high-grade melt-bearing metapelitic rocks derived in two stages from | 100 | high-grade melt-bearing metapelitic rocks derived in two stages from | ||
| 91 | metasediments surrounding crustal magma chambers. Microstructures and | 101 | metasediments surrounding crustal magma chambers. Microstructures and | ||
| 92 | age relationships indicate that a first stage of migmatization and | 102 | age relationships indicate that a first stage of migmatization and | ||
| 93 | melt extraction was overprinted by a sequence of melt-bearing reaction | 103 | melt extraction was overprinted by a sequence of melt-bearing reaction | ||
| 94 | microstructures. The preservation of melt as glass requires only a | 104 | microstructures. The preservation of melt as glass requires only a | ||
| 95 | short residence time before eruption of the xenoliths in the host | 105 | short residence time before eruption of the xenoliths in the host | ||
| 96 | melt. The P-T conditions of the melting processes have been | 106 | melt. The P-T conditions of the melting processes have been | ||
| 97 | constrained by metamorphic modelling of mineral assemblages, phase | 107 | constrained by metamorphic modelling of mineral assemblages, phase | ||
| 98 | compositions and reaction sequences in local compositional domains in | 108 | compositions and reaction sequences in local compositional domains in | ||
| 99 | the system NCKFMASHTO using THERMOCALC software. The calculations | 109 | the system NCKFMASHTO using THERMOCALC software. The calculations | ||
| 100 | predict that within the El Hoyazo and Mazarron volcanic suites, | 110 | predict that within the El Hoyazo and Mazarron volcanic suites, | ||
| 101 | Grt-Bt-Sil (+/- Crd, Pl) enclaves containing a distinctive | 111 | Grt-Bt-Sil (+/- Crd, Pl) enclaves containing a distinctive | ||
| 102 | fibrolite-melt intergrowth formed over the temperature range 700-770 | 112 | fibrolite-melt intergrowth formed over the temperature range 700-770 | ||
| 103 | degrees C at 5 kbar, and that these were overprinted by corona | 113 | degrees C at 5 kbar, and that these were overprinted by corona | ||
| 104 | structures around garnet containing Spl-Crd-Kfs-melt at 775 degrees C, | 114 | structures around garnet containing Spl-Crd-Kfs-melt at 775 degrees C, | ||
| 105 | 4 center dot 8 kbar, and newly grown spinel with melt haloes (only at | 115 | 4 center dot 8 kbar, and newly grown spinel with melt haloes (only at | ||
| 106 | El Hoyazo) at 835 degrees C and 5 center dot 8 kbar. At Mar Menor, the | 116 | El Hoyazo) at 835 degrees C and 5 center dot 8 kbar. At Mar Menor, the | ||
| 107 | xenoliths show garnet replaced by Opx, Crd, Spl and melt at 810-840 | 117 | xenoliths show garnet replaced by Opx, Crd, Spl and melt at 810-840 | ||
| 108 | degrees C, 2-2 center dot 5 kbar; aluminous xenoliths containing | 118 | degrees C, 2-2 center dot 5 kbar; aluminous xenoliths containing | ||
| 109 | andalusite were replaced by Spl + Crd under the same conditions. The | 119 | andalusite were replaced by Spl + Crd under the same conditions. The | ||
| 110 | P-T distribution, size and relative abundance of the various xenolith | 120 | P-T distribution, size and relative abundance of the various xenolith | ||
| 111 | types are best explained by the formation of the melt-bearing | 121 | types are best explained by the formation of the melt-bearing | ||
| 112 | assemblages in a transiently heated wall-rock profile adjacent to a | 122 | assemblages in a transiently heated wall-rock profile adjacent to a | ||
| 113 | magma chamber or conduit, followed by collapse of the wall and brief | 123 | magma chamber or conduit, followed by collapse of the wall and brief | ||
| 114 | residence of the resulting fragments as xenoliths in a dacitic magma | 124 | residence of the resulting fragments as xenoliths in a dacitic magma | ||
| 115 | at c. 850 degrees C. The difference in pressure between the locations | 125 | at c. 850 degrees C. The difference in pressure between the locations | ||
| 116 | reflects the depth of magma chambers in the crust. The predominance of | 126 | reflects the depth of magma chambers in the crust. The predominance of | ||
| 117 | smaller, hotter enclaves in the Mar Menor occurrence may reflect less | 127 | smaller, hotter enclaves in the Mar Menor occurrence may reflect less | ||
| 118 | favourable conditions for developing thermally softened wall-rock | 128 | favourable conditions for developing thermally softened wall-rock | ||
| 119 | profiles along high thermal gradients at shallower depth.", | 129 | profiles along high thermal gradients at shallower depth.", | ||
| 120 | "notes_translated": { | 130 | "notes_translated": { | ||
| 121 | "es": "Crustal xenoliths from the Neogene Volcanic Province (NVP) | 131 | "es": "Crustal xenoliths from the Neogene Volcanic Province (NVP) | ||
| 122 | of the Betic Cordillera, SE Spain, constitute an unusual suite of | 132 | of the Betic Cordillera, SE Spain, constitute an unusual suite of | ||
| 123 | high-grade melt-bearing metapelitic rocks derived in two stages from | 133 | high-grade melt-bearing metapelitic rocks derived in two stages from | ||
| 124 | metasediments surrounding crustal magma chambers. Microstructures and | 134 | metasediments surrounding crustal magma chambers. Microstructures and | ||
| 125 | age relationships indicate that a first stage of migmatization and | 135 | age relationships indicate that a first stage of migmatization and | ||
| 126 | melt extraction was overprinted by a sequence of melt-bearing reaction | 136 | melt extraction was overprinted by a sequence of melt-bearing reaction | ||
| 127 | microstructures. The preservation of melt as glass requires only a | 137 | microstructures. The preservation of melt as glass requires only a | ||
| 128 | short residence time before eruption of the xenoliths in the host | 138 | short residence time before eruption of the xenoliths in the host | ||
| 129 | melt. The P-T conditions of the melting processes have been | 139 | melt. The P-T conditions of the melting processes have been | ||
| 130 | constrained by metamorphic modelling of mineral assemblages, phase | 140 | constrained by metamorphic modelling of mineral assemblages, phase | ||
| 131 | compositions and reaction sequences in local compositional domains in | 141 | compositions and reaction sequences in local compositional domains in | ||
| 132 | the system NCKFMASHTO using THERMOCALC software. The calculations | 142 | the system NCKFMASHTO using THERMOCALC software. The calculations | ||
| 133 | predict that within the El Hoyazo and Mazarron volcanic suites, | 143 | predict that within the El Hoyazo and Mazarron volcanic suites, | ||
| 134 | Grt-Bt-Sil (+/- Crd, Pl) enclaves containing a distinctive | 144 | Grt-Bt-Sil (+/- Crd, Pl) enclaves containing a distinctive | ||
| 135 | fibrolite-melt intergrowth formed over the temperature range 700-770 | 145 | fibrolite-melt intergrowth formed over the temperature range 700-770 | ||
| 136 | degrees C at 5 kbar, and that these were overprinted by corona | 146 | degrees C at 5 kbar, and that these were overprinted by corona | ||
| 137 | structures around garnet containing Spl-Crd-Kfs-melt at 775 degrees C, | 147 | structures around garnet containing Spl-Crd-Kfs-melt at 775 degrees C, | ||
| 138 | 4 center dot 8 kbar, and newly grown spinel with melt haloes (only at | 148 | 4 center dot 8 kbar, and newly grown spinel with melt haloes (only at | ||
| 139 | El Hoyazo) at 835 degrees C and 5 center dot 8 kbar. At Mar Menor, the | 149 | El Hoyazo) at 835 degrees C and 5 center dot 8 kbar. At Mar Menor, the | ||
| 140 | xenoliths show garnet replaced by Opx, Crd, Spl and melt at 810-840 | 150 | xenoliths show garnet replaced by Opx, Crd, Spl and melt at 810-840 | ||
| 141 | degrees C, 2-2 center dot 5 kbar; aluminous xenoliths containing | 151 | degrees C, 2-2 center dot 5 kbar; aluminous xenoliths containing | ||
| 142 | andalusite were replaced by Spl + Crd under the same conditions. The | 152 | andalusite were replaced by Spl + Crd under the same conditions. The | ||
| 143 | P-T distribution, size and relative abundance of the various xenolith | 153 | P-T distribution, size and relative abundance of the various xenolith | ||
| 144 | types are best explained by the formation of the melt-bearing | 154 | types are best explained by the formation of the melt-bearing | ||
| 145 | assemblages in a transiently heated wall-rock profile adjacent to a | 155 | assemblages in a transiently heated wall-rock profile adjacent to a | ||
| 146 | magma chamber or conduit, followed by collapse of the wall and brief | 156 | magma chamber or conduit, followed by collapse of the wall and brief | ||
| 147 | residence of the resulting fragments as xenoliths in a dacitic magma | 157 | residence of the resulting fragments as xenoliths in a dacitic magma | ||
| 148 | at c. 850 degrees C. The difference in pressure between the locations | 158 | at c. 850 degrees C. The difference in pressure between the locations | ||
| 149 | reflects the depth of magma chambers in the crust. The predominance of | 159 | reflects the depth of magma chambers in the crust. The predominance of | ||
| 150 | smaller, hotter enclaves in the Mar Menor occurrence may reflect less | 160 | smaller, hotter enclaves in the Mar Menor occurrence may reflect less | ||
| 151 | favourable conditions for developing thermally softened wall-rock | 161 | favourable conditions for developing thermally softened wall-rock | ||
| 152 | profiles along high thermal gradients at shallower depth." | 162 | profiles along high thermal gradients at shallower depth." | ||
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