Geodynamics of continental rift initiation and evolution
A continental rift is a nascent plate boundary where the lithosphere is thinned by tectonic
activity. Some continental rifts undergo extension to the point that they generate a new …
activity. Some continental rifts undergo extension to the point that they generate a new …
No single model for supersized eruptions and their magma bodies
Supereruptions are the largest explosive volcanic eruptions on Earth. They generate
catastrophic, widespread ash-fall blankets and voluminous ignimbrites, with accompanying …
catastrophic, widespread ash-fall blankets and voluminous ignimbrites, with accompanying …
Hydrologic, magmatic, and tectonic controls on hydrothermal flow, Taupo Volcanic Zone, New Zealand: Implications for the formation of epithermal vein deposits
JV Rowland, SF Simmons - Economic Geology, 2012 - pubs.geoscienceworld.org
Geologic controls on development of high-flux hydrothermal conduits that promote
epithermal ore formation are evaluated at large and small scales for geothermal systems of …
epithermal ore formation are evaluated at large and small scales for geothermal systems of …
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 …
world's most spectacular and productive areas of Quaternary silicic volcanism and …
A model of active faulting in New Zealand
Active fault traces are a surface expression of permanent deformation that accommodates
the motion within and between adjacent tectonic plates. We present an updated national …
the motion within and between adjacent tectonic plates. We present an updated national …
Taupō: an overview of New Zealand's youngest supervolcano
ABSTRACT Taupō volcano (New Zealand) is distinguished as the source of Earth's
youngest supereruption (∼ 25.5 ka), with Lake Taupō occupying the resulting caldera …
youngest supereruption (∼ 25.5 ka), with Lake Taupō occupying the resulting caldera …
From mush to eruption in centuries: assembly of the super-sized Oruanui magma body
ASR Allan, DJ Morgan, CJN Wilson… - Contributions to Mineralogy …, 2013 - Springer
The magmatic systems that give rise to voluminous crystal-poor rhyolite magma bodies can
be considered to operate on two contrasting timescales: Those governed by longer-term …
be considered to operate on two contrasting timescales: Those governed by longer-term …
Volcanic activity and hazard in the East African Rift Zone
Over the past two decades, multidisciplinary studies have unearthed a rich history of
volcanic activity and unrest in the densely-populated East African Rift System, providing new …
volcanic activity and unrest in the densely-populated East African Rift System, providing new …
[图书][B] Geology of the Rotorua area
GS Leonard, JG Begg, CJN Wilson, GS Leonard - 2010 - researchgate.net
1The QMAP Quaternary timescale pre-dates the presently recognised chronology for the
Pleistocene/Quaternary. QMAP adopted the Quaternary Period in 1994, based definitions on …
Pleistocene/Quaternary. QMAP adopted the Quaternary Period in 1994, based definitions on …
Thermomechanical feedbacks in magmatic systems: Implications for growth, longevity, and evolution of large caldera-forming magma reservoirs and their …
SL de Silva, PM Gregg - Journal of Volcanology and Geothermal Research, 2014 - Elsevier
Large magma bodies that feed super-eruptions and build batholiths are not instantaneously
emplaced. Many accumulate over time scales of 10 5 to 10 6 years as part of magmatic …
emplaced. Many accumulate over time scales of 10 5 to 10 6 years as part of magmatic …