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 …
the central part of the Taupo Volcanic Zone, New Zealand. During its~ 625 kyr volcanic …
Mechanical and physical properties of hydrothermally altered rocks, Taupo Volcanic Zone, New Zealand
LD Wyering, MC Villeneuve, IC Wallis… - Journal of Volcanology …, 2014 - Elsevier
Mechanical characterization of hydrothermally altered rocks from geothermal reservoirs will
lead to an improved understanding of rock mechanics in a geothermal environment. To …
lead to an improved understanding of rock mechanics in a geothermal environment. To …
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 …
[HTML][HTML] Fault ruptures triggered by large rhyolitic eruptions at the boundary between tectonic and magmatic rift segments: The Manawahe Fault, Taupō Rift, New …
P Villamor, NJ Litchfield, D Gómez-Ortiz… - Journal of Volcanology …, 2022 - Elsevier
Abstract The Manawahe Fault is located at the boundary between the tectonic Whakatane
and the magmatic Okataina segments of the Taupō Rift. We investigate prehistoric ground …
and the magmatic Okataina segments of the Taupō Rift. We investigate prehistoric ground …
[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 …
Spatial and temporal variations in magma-assisted rifting, Taupo Volcanic Zone, New Zealand
Taupo Volcanic Zone (TVZ), New Zealand, is a NNE-trending rifting arc, active for~ 2 Myr,
with a 125-km-long central segment characterized by exceptionally voluminous rhyolite …
with a 125-km-long central segment characterized by exceptionally voluminous rhyolite …
The integrated history of repeated caldera formation and infill at the Okataina Volcanic Centre: Insights from 3D gravity and magnetic models
CA Miller, J Barretto, V Stagpoole… - Journal of Volcanology …, 2022 - Elsevier
Multistage collapse caldera create complex geological structures that are often buried by
kilometers of pyroclastic infill and late stage lava domes, making study of their origins difficult …
kilometers of pyroclastic infill and late stage lava domes, making study of their origins difficult …
Imaging sub-caldera structure with local seismicity, Okataina Volcanic Centre, Taupo Volcanic Zone, using double-difference seismic tomography
We examine sub-caldera structure and seismicity in and around the Okataina Volcanic
Centre (OVC), Taupo Volcanic Zone, New Zealand, using seismic data collected over 4+ …
Centre (OVC), Taupo Volcanic Zone, New Zealand, using seismic data collected over 4+ …
Extraction, storage and eruption of multiple isolated magma batches in the paired Mamaku and Ohakuri eruption, Taupo Volcanic Zone, New Zealand
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 …
magma generation and caldera-forming eruptions. Less is known about how large volumes …
Structure and kinematics of the Taupo rift, New Zealand
The structure and kinematics of the continental intra‐arc Taupo Rift have been constrained
by fault‐trace mapping, a large catalogue of focal mechanisms (N= 202) and fault slip …
by fault‐trace mapping, a large catalogue of focal mechanisms (N= 202) and fault slip …