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 …
1The QMAP Quaternary timescale pre-dates the presently recognised chronology for the Pleistocene/Quaternary. QMAP adopted the Quaternary Period in 1994, based definitions on …
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 …
Fault interactions are an essential feature of all fault systems on timescales of individual earthquakes to millions of years. We examine the role of these interactions in the …
Displacements on tectonic faults primarily accrue during earthquakes at rates that vary through time. To examine the processes that underlie the temporal changes in fault …
The evolution of the continental intraarc Taupo Rift in the North Island, New Zealand, is rapid, significantly faster than comparative intracontinental rifts such as the African Rifts …
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 …
JW Cole, KD Spinks, CD Deering, IA Nairn… - Journal of volcanology …, 2010 - Elsevier
The Okataina Volcanic Centre (OVC) contains the northeasternmost caldera complex in onshore Taupo Volcanic Zone (TVZ), New Zealand, sited largely within the Taupo Rift …
CK Morley - Journal of Asian Earth Sciences, 2013 - Elsevier
Understanding the roles of Cenozoic strike-slip faults in SE Asia observed in outcrop onshore, with their offshore continuation has produced a variety of structural models …