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Open AccessReported ultra-low lava viscosities from the 2021 La Palma eruption are potentially biased
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Open AccessHidden mechanical weaknesses within lava domes provided by buried high-porosity hydrothermal alteration zones
Catastrophic lava dome collapse is considered an unpredictable volcanic hazard because the physical properties, stress conditions, and internal structure of lava domes are not well understood and can change ra...
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Open AccessSunda arc mantle source δ18O value revealed by intracrystal isotope analysis
Magma plumbing systems underlying subduction zone volcanoes extend from the mantle through the overlying crust and facilitate protracted fractional crystallisation, assimilation, and mixing, which frequently o...
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Open AccessConstraining the sub-arc, parental magma composition for the giant Altiplano-Puna Volcanic Complex, northern Chile
The Andean continental arc is built upon the thickest crust on Earth, whose eruption products reflect varying degrees of crustal assimilation. In order to robustly model magma evolution and assimilation at sub...
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Open AccessHydrothermal alteration of andesitic lava domes can lead to explosive volcanic behaviour
Dome-forming volcanoes are among the most hazardous volcanoes on Earth. Magmatic outgassing can be hindered if the permeability of a lava dome is reduced, promoting pore pressure augmentation and explosive beh...
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Open AccessInteraction between high-temperature magmatic fluids and limestone explains ‘Bastnäs-type’ REE deposits in central Sweden
The presently increasing demand for rare earth elements (REE), particularly in high-tech and “green energy” applications, has led to global interest in the distribution, origins and formation conditions of REE...
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Open AccessComplex hazard cascade culminating in the Anak Krakatau sector collapse
Flank instability and sector collapses, which pose major threats, are common on volcanic islands. On 22 Dec 2018, a sector collapse event occurred at Anak Krakatau volcano in the Sunda Strait, triggering a dea...
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Open AccessCrustal CO2 contribution to subduction zone degassing recorded through calc-silicate xenoliths in arc lavas
Interaction between magma and crustal carbonate at active arc volcanoes has recently been proposed as a source of atmospheric CO2, in addition to CO2 released from the mantle and subducted oceanic crust. However,...
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Open AccessGlobal Fe–O isotope correlation reveals magmatic origin of Kiruna-type apatite-iron-oxide ores
Kiruna-type apatite-iron-oxide ores are key iron sources for modern industry, yet their origin remains controversial. Diverse ore-forming processes have been discussed, comprising low-temperature hydrothermal ...
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Open AccessA large explosive silicic eruption in the British Palaeogene Igneous Province
Large-volume pyroclastic eruptions are not known from the basalt-dominated British Palaeogene Igneous Province (BPIP), although silicic magmatism is documented from intra-caldera successions in central volcano...
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Open AccessMulti-level magma plumbing at Agung and Batur volcanoes increases risk of hazardous eruptions
The island of Bali in Indonesia is home to two active stratovolcanoes, Agung and Batur, but relatively little is known of their underlying magma plumbing systems. Here we define magma storage depths and isotop...
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Open AccessMagma reservoir dynamics at Toba caldera, Indonesia, recorded by oxygen isotope zoning in quartz
Quartz is a common phase in high-silica igneous rocks and is resistant to post-eruptive alteration, thus offering a reliable record of magmatic processes in silicic magma systems. Here we employ the 75 ka Toba...
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Open AccessErupted frothy xenoliths may explain lack of country-rock fragments in plutons
Magmatic sto** is discussed to be a main mechanism of magma emplacement. As a consequence of sto**, abundant country-rock fragments should occur within and at the bottom of, magma reservoirs as “xenolith g...
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Open AccessLocating the depth of magma supply for volcanic eruptions, insights from Mt. Cameroon
Mt. Cameroon is one of the most active volcanoes in Africa and poses a possible threat to about half a million people in the area, yet knowledge of the volcano’s underlying magma supply system is sparse. To ch...
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Open AccessBoron isotope fractionation in magma via crustal carbonate dissolution
Carbon dioxide released by arc volcanoes is widely considered to originate from the mantle and from subducted sediments. Fluids released from upper arc carbonates, however, have recently been proposed to help ...
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Open AccessMagma transport in sheet intrusions of the Alnö carbonatite complex, central Sweden
Magma transport through the Earth’s crust occurs dominantly via sheet intrusions, such as dykes and cone-sheets and is fundamental to crustal evolution, volcanic eruptions and geochemical element cycling. Howe...
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Open AccessNannofossils in 2011 El Hierro eruptive products reinstate plume model for Canary Islands
The origin and life cycle of ocean islands have been debated since the early days of Geology. In the case of the Canary archipelago, its proximity to the Atlas orogen led to initial fracture-controlled models ...
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Open AccessWeibull-distributed dyke thickness reflects probabilistic character of host-rock strength
Magmatic sheet intrusions (dykes) constitute the main form of magma transport in the Earth’s crust. The size distribution of dykes is a crucial parameter that controls volcanic surface deformation and eruption...
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Open AccessArdnamurchan 3D cone-sheet architecture explained by a single elongate magma chamber
The Palaeogene Ardnamurchan central igneous complex, NW Scotland, was a defining place for the development of the classic concepts of cone-sheet and ring-dyke emplacement and has thus fundamentally influenced ...
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Open AccessCarbonatite ring-complexes explained by caldera-style volcanism
Carbonatites are rare, carbonate-rich magmatic rocks that make up a minute portion of the crust only, yet they are of great relevance for our understanding of crustal and mantle processes. Although they occur ...