Magma residence time, ascent rate and eruptive style of the November ash-laden activity during the 2021 Tajogaite eruption (La Palma, Spain)

被引:7
作者
Bonechi, Barbara [1 ]
Polacci, Margherita [1 ]
Arzilli, Fabio [2 ]
Romero, Jorge E. [3 ]
Fellowes, Jonathan [1 ]
Burton, Mike [1 ]
机构
[1] Univ Manchester, Dept Earth & Environm Sci, Manchester, England
[2] Sch Sci & Technol, Geol Div, Camerino, Italy
[3] Univ OHiggins, Inst Ciencias Ingn, Rancagua, Chile
来源
VOLCANICA | 2024年 / 7卷 / 01期
关键词
Pre-eruptive conditions; Basanitic melt; Crystal size distribution; Geothermobarometry; Ash-rich jets; Eruptive style; INDUCED CRYSTALLIZATION; BASALTIC SCORIA; ROCKS; THERMOBAROMETRY; EVOLUTION; PETROLOGY; DYNAMICS; KINETICS; STORAGE;
D O I
10.30909/vol.07.01.5165
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We combined compositional analyses, crystal size distributions and geothermobarometry of tephra erupted during the 2021 Tajogaite eruption (La Palma, Spain), focusing on samples collected in November 2021 associated with a period of abundant ash emission characteristic of the second half of the eruption (from October onwards). Magma erupted in November exhibits a more primitive basanitic composition than the earlier magma. Crystallisation temperatures range between 1100-1160 degrees C (H2O 2 O = 1-3 wt.degrees%o) for phenocrysts and microphenocrysts, with corresponding pressures indicating depths from 10 to 30 km. Crystal size distribution analysis reveals short (minutes) residence times for plagioclase. Finally, magma ascent velocities ( 0.01-0.3 m s-1) - 1 ) suggest acceleration and fragmentation in the shallowest part of the conduit. Our results suggest that the trigger of the November explosive activity can be attributed to complex feedback between gas emission rates, changes in conduit geometry, and magma ascent rate.
引用
收藏
页码:51 / 65
页数:15
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