2021 年塔霍加岩喷发期间 11 月火山灰活动的岩浆停留时间、上升速度和喷发方式(西班牙拉帕尔马)

IF 2.5 Q2 Earth and Planetary Sciences
Volcanica Pub Date : 2024-01-31 DOI:10.30909/vol.07.01.5165
B. Bonechi, M. Polacci, F. Arzilli, Jorge Romero, Jonathan Fellowes, M. Burton
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引用次数: 0

摘要

我们将 2021 年塔霍加岩喷发(西班牙拉帕尔马)期间喷发的表灰的成分分析、晶体尺寸分布和地温测量法结合起来,重点研究了 2021 年 11 月采集的样本,这些样本与喷发后半期(从 10 月开始)的大量火山灰喷发期有关。与早期岩浆相比,11 月份喷发的岩浆呈现出更原始的玄武岩成分。表晶和微表晶的结晶温度介于约1100-1160 °C(H2O = 1-3重量%)之间,相应的压力显示深度为约10-约30千米。晶体尺寸分布分析显示斜长石的停留时间很短(几分钟)。最后,岩浆上升速度(约 0.01-0.3 米/秒-1)表明在导管的最浅部分发生了加速和碎裂。我们的研究结果表明,11月爆炸活动的触发可归因于气体排放率、导管几何形状变化和岩浆上升速度之间的复杂反馈。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Magma residence time, ascent rate and eruptive style of the November ash-laden activity during the 2021 Tajogaite eruption (La Palma, Spain)
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 °C (H2O = 1–3 wt.%) 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) 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.
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来源期刊
Volcanica
Volcanica Earth and Planetary Sciences-Geology
CiteScore
4.40
自引率
0.00%
发文量
21
审稿时长
21 weeks
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