National seismic hazard model for New Zealand: 2010 update
M Stirling, G McVerry… - Bulletin of the …, 2012 - pubs.geoscienceworld.org
A team of earthquake geologists, seismologists, and engineering seismologists has
collectively produced an update of the national probabilistic seismic hazard (PSH) model for …
collectively produced an update of the national probabilistic seismic hazard (PSH) model for …
The conundrums of the postglacial tectonic response of the Fennoscandian and Canadian Shields
H Bungum, O Eldholm - Earth-Science Reviews, 2022 - Elsevier
A review of the early Holocene paleoseismicity in areas covered by huge ice sheets in the
interior of Fennoscandia and North America shows that observational data and numerical …
interior of Fennoscandia and North America shows that observational data and numerical …
Seismic hazard analyses from geologic and geomorphic data: Current and future challenges
The loss of life and economic consequences caused by several recent earthquakes
demonstrate the importance of developing seismically safe building codes. The …
demonstrate the importance of developing seismically safe building codes. The …
Normal fault interactions, paleoearthquakes and growth in an active rift
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 …
earthquakes to millions of years. We examine the role of these interactions in the …
Fault displacement rates on a range of timescales
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 …
through time. To examine the processes that underlie the temporal changes in fault …
Rapid evolution of subduction‐related continental intraarc rifts: The Taupo Rift, New Zealand
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 …
rapid, significantly faster than comparative intracontinental rifts such as the African Rifts …
Integrating faults and past earthquakes into a probabilistic seismic hazard model for peninsular Italy
Italy is one of the most seismically active countries in Europe. Moderate to strong
earthquakes, with magnitudes of up to∼ 7, have been historically recorded for many active …
earthquakes, with magnitudes of up to∼ 7, have been historically recorded for many active …
The Dinaric fault system: Large‐scale structure, rates of slip, and Plio‐Pleistocene evolution of the transpressive northeastern boundary of the Adria microplate
Located at the northeastern corner of the Adria microplate, the Alps‐Dinarides junction
represents a key region for understanding how the Adria microplate interacts with stable …
represents a key region for understanding how the Adria microplate interacts with stable …
Relationships between fault geometry, slip rate variability and earthquake recurrence in extensional settings
Field observations and modelling indicate that elastic interaction between active faults can
lead to variations in earthquake recurrence intervals measured on timescales of 102-104 yr …
lead to variations in earthquake recurrence intervals measured on timescales of 102-104 yr …
Late Quaternary slip rates for the Hyde and Dunstan faults, southern New Zealand: Implications for strain migration in a slowly deforming continental plate margin
Reverse faulting in Otago, southern New Zealand, accommodates distributed tectonic
convergence on the eastern side of the Australian‐Pacific plate boundary. Paleoearthquake …
convergence on the eastern side of the Australian‐Pacific plate boundary. Paleoearthquake …