Search Results - "Wilson, Colin J. N"
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Volcanic glass from the 1.8 ka Taupō eruption (New Zealand) detected in Antarctic ice at ~ 230 CE
Published in Scientific reports (09-10-2023)“…Chemical anomalies in polar ice core records are frequently linked to volcanism; however, without the presence of (crypto)tephra particles, links to specific…”
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Growth of volcanic ash aggregates in the presence of liquid water and ice: an experimental approach
Published in Bulletin of volcanology (01-11-2012)“…Key processes influencing the aggregation of volcanic ash and hydrometeors are examined with an experimental method employing vibratory pan aggregation…”
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Fine-scale temporal recovery, reconstruction and evolution of a post-supereruption magmatic system
Published in Contributions to mineralogy and petrology (01-07-2015)“…Supereruptions (>10 15 kg ≈ 450 km 3 of ejected magma) have received much attention because of the challenges in explaining how and over what time intervals…”
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Contrasting pyroclast density spectra from subaerial and submarine silicic eruptions in the Kermadec arc: implications for eruption processes and dredge sampling
Published in Bulletin of volcanology (01-08-2012)“…Pyroclastic deposits from four caldera volcanoes in the Kermadec arc have been sampled from subaerial sections (Raoul and Macauley) and by dredging from the…”
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Highly vesicular pumice generated by buoyant detachment of magma in subaqueous volcanism
Published in Nature geoscience (01-02-2013)“…Deposits of highly vesicular pumice that blanket submarine volcanoes are often attributed to explosive eruptions. Density and textural analysis of clasts…”
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Eruptive and environmental processes recorded by diatoms in volcanically dispersed lake sediments from the Taupo Volcanic Zone, New Zealand
Published in Journal of paleolimnology (01-12-2015)“…Late Pleistocene diatomaceous sediment was widely dispersed along with volcanic ash (tephra) across and beyond New Zealand by the 25.4 ka Oruanui supereruption…”
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From mush to eruption in centuries: assembly of the super-sized Oruanui magma body
Published in Contributions to mineralogy and petrology (01-07-2013)“…The magmatic systems that give rise to voluminous crystal-poor rhyolite magma bodies can be considered to operate on two contrasting timescales: Those governed…”
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A cascade of magmatic events during the assembly and eruption of a super-sized magma body
Published in Contributions to mineralogy and petrology (01-07-2017)“…We use comprehensive geochemical and petrological records from whole-rock samples, crystals, matrix glasses and melt inclusions to derive an integrated picture…”
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A sulfur and halogen budget for the large magmatic system beneath Taupō volcano
Published in Contributions to mineralogy and petrology (01-10-2022)“…The transport and degassing pathways of volatiles through large silicic magmatic systems are central to understanding geothermal fluid compositions, ore…”
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Volcanic Unrest at Taupō Volcano in 2019: Causes, Mechanisms and Implications
Published in Geochemistry, geophysics, geosystems : G3 (01-06-2021)“…Abstract Taupō volcano, New Zealand, is a large caldera volcano that has been highly active through the Holocene. It most recently erupted ∼1,800 years ago but…”
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New Zealand supereruption provides time marker for the Last Glacial Maximum in Antarctica
Published in Scientific reports (25-09-2017)“…Multiple, independent time markers are essential to correlate sediment and ice cores from the terrestrial, marine and glacial realms. These records constrain…”
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Tracking Magma‐Crust‐Fluid Interactions at High Temporal Resolution: Oxygen Isotopes in Young Silicic Magmas of the Taupō Volcanic Zone
Published in Geochemistry, geophysics, geosystems : G3 (01-01-2023)“…Oxygen isotopes are useful for tracing interactions between magmas, crustal rocks and surface‐derived waters. We use them here to consider links between…”
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Evacuation of multiple magma bodies and the onset of caldera collapse in a supereruption, captured in glass and mineral compositions
Published in Contributions to mineralogy and petrology (01-04-2018)“…Complexities in the nature of large-scale silicic eruptions and their magmatic systems can be discerned through micro-analytical geochemical studies. We…”
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Wiggle-match radiocarbon dating of the Taupo eruption
Published in Nature communications (11-10-2019)Get full text
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The Mesozoic terrane boundary beneath the Taupo Volcanic Zone, New Zealand, and potential controls on geothermal system characteristics
Published in New Zealand journal of geology and geophysics (02-10-2021)“…The Taupo Volcanic Zone (TVZ) in the central North Island of New Zealand lies across the boundary formed in the late Mesozoic between two major basement…”
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Melt pockets in phenocrysts and decompression rates of silicic magmas before fragmentation
Published in Journal of Geophysical Research - Solid Earth (01-06-2007)“…A new method is presented to estimate the decompression rate of silicic magma prior to fragmentation and is applicable to rates of 1–100 kPa/s. This method…”
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Textural and micro-analytical insights into mafic–felsic interactions during the Oruanui eruption, Taupo
Published in Contributions to mineralogy and petrology (01-05-2018)“…Quenched juvenile mafic inclusions (enclaves) are an occasional but informative component in the deposits of large felsic eruptions. Typically, the…”
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Palaeotemperature determinations for the 1.8-ka Taupo ignimbrite, New Zealand, and implications for the emplacement history of a high-velocity pyroclastic flow
Published in Bulletin of volcanology (01-08-2004)“…Palaeomagnetic data from lithic clasts collected at 46 sites within layers 1 and 2 of the 1.8-ka Taupo ignimbrite, New Zealand, have been used to determine the…”
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The nature, origins and distribution of ash aggregates in a large-scale wet eruption deposit: Oruanui, New Zealand
Published in Journal of volcanology and geothermal research (15-01-2013)“…This study documents the processes and products of volcanic ash aggregation in phreatomagmatic phases of the 25.4ka Oruanui supereruption from Taupo volcano,…”
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Diverse patterns of ascent, degassing, and eruption of rhyolite magma during the 1.8 ka Taupo eruption, New Zealand: Evidence from clast vesicularity
Published in Journal of volcanology and geothermal research (10-08-2010)“…The 22 km 3 (DRE) 1.8 ka Taupo eruption ejected chemically uniform rhyolite in a wide range of eruptive styles and intensities. The 7 eruptive units include…”
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