Remelting of cumulates as a process for producing chemical zoning in silicic tuffs: A comparison of cool, wet and hot, dry rhyolitic magma systems

JA Wolff, BS Ellis, FC Ramos, WA Starkel, S Boroughs… - Lithos, 2015 - Elsevier
We review petrological and geochemical features of silicic pyroclastic deposits of dominantly
low to moderate (0–25%) crystallinity, and volumes in the range of 5–1000 km 3, erupted …

How are silicic volcanic and plutonic systems related? Part 1: A review of geological and geophysical observations, and insights from igneous rock chemistry

JD Clemens, SE Bryan, MJ Mayne, G Stevens… - Earth-Science …, 2022 - Elsevier
Silicic volcanic and plutonic rocks (SiO 2≥ 66 wt%) are generally viewed as being either
compositional equivalents or complementary to each other. However, consideration of the …

The volcanic, magmatic and tectonic setting of the Taupo Volcanic Zone, New Zealand, reviewed from a geothermal perspective

CJN Wilson, JV Rowland - Geothermics, 2016 - Elsevier
Abstract The Taupo Volcanic Zone (TVZ) in the North Island of New Zealand is one of the
world's most spectacular and productive areas of Quaternary silicic volcanism and …

Trace element indicators of crystal accumulation in silicic igneous rocks

CD Deering, O Bachmann - Earth and Planetary Science Letters, 2010 - Elsevier
If fractional crystallization coupled with some crustal assimilation (AFC) is the dominant
process for generating evolved magmas in the Earth's crust, large quantities of igneous …

[HTML][HTML] Magma reservoir evolution during the build up to and recovery from caldera-forming eruptions–a generalizable model?

CB de Maisonneuve, F Forni, O Bachmann - Earth-Science Reviews, 2021 - Elsevier
Silicic calderas globally tend to record a cyclic magmatic, structural, and eruptive
evolutionary progression. Some calderas are polycyclic, involving multiple catastrophic …

Rift-related transition from andesite to rhyolite volcanism in the Taupo Volcanic Zone (New Zealand) controlled by crystal–melt dynamics in mush zones with variable …

CD Deering, O Bachmann, J Dufek… - Journal of …, 2011 - academic.oup.com
Abstract The Taupo Volcanic Zone (TVZ), located in the North Island of New Zealand,
represents part of a magmatic arc that is at present undergoing active extension. Around 0· 9 …

Origin of heavy Fe isotope compositions in high-silica igneous rocks: A rhyolite perspective

DH Du, XL Wang, T Yang, X Chen, JY Li… - … et Cosmochimica Acta, 2017 - Elsevier
The origin of heavy Fe isotope compositions in high-silica (> 70 wt% SiO 2) igneous rocks
remains a highly controversial topic. Considering that fluid exsolution in eruptive rocks is …

Following magma: the pathway of silicic magmas from extraction to storage during an ignimbrite flare-up, Taupō volcanic zone, New Zealand

SL Smithies, LJ Harmon, SM Allen, DM Gravley… - Earth and Planetary …, 2023 - Elsevier
Very large silicic magma systems can generate tens to thousands of cubic kilometres of very
evolved, rhyolitic magmas that erupt in caldera-forming events. These magma systems may …

Extraction, storage and eruption of multiple isolated magma batches in the paired Mamaku and Ohakuri eruption, Taupo Volcanic Zone, New Zealand

F Bégué, CD Deering, DM Gravley… - Journal of …, 2014 - academic.oup.com
Abstract The Taupo Volcanic Zone (TVZ) is well known for its extraordinary rate of rhyolitic
magma generation and caldera-forming eruptions. Less is known about how large volumes …

Okataina Volcanic Centre, Taupo Volcanic Zone, New Zealand: A review of volcanism and synchronous pluton development in an active, dominantly silicic caldera …

JW Cole, CD Deering, RM Burt, S Sewell… - Earth-Science …, 2014 - Elsevier
Abstract The Okataina Volcanic Centre (OVC) is one of eight caldera systems, which form
the central part of the Taupo Volcanic Zone, New Zealand. During its~ 625 kyr volcanic …