Earthquakes triggered by fluid diffusion and boosted by fault reactivation in Weiyuan, China due to hydraulic fracturing

M Sheng, R Chu, Z Peng, Z Wei, X Zeng… - Journal of …, 2022 - Wiley Online Library
Hydraulic fracturing has induced small‐to‐moderate‐size earthquakes around the world.
Identifying spatio‐temporal evolution of microseismicity is important for understanding the …

Relocation of the Foreshocks and Aftershocks of the 2021 Ms 6.4 Yangbi Earthquake Sequence, Yunnan, China

T Yang, B Li, L Fang, Y Su, Y Zhong, J Yang… - Journal of Earth …, 2022 - Springer
An M s 6.4 earthquake occurred in Yangbi, Yunnan, China on May 21, 2021, which has
obvious foreshock activity and abundant aftershocks. Based on the seismic observation data …

New Zealand fault‐rupture depth model v. 1.0: A provisional estimate of the maximum depth of seismic rupture on New Zealand's active faults

S Ellis, S Bannister, R Van Dissen… - Bulletin of the …, 2024 - pubs.geoscienceworld.org
We summarize estimates of the maximum rupture depth on New Zealand's active faults
(“New Zealand Fault‐Rupture Depth Model v. 1.0”), as used in the New Zealand Community …

A review of the 2016 Kaikōura earthquake: insights from the first 3 years

IJ Hamling - Journal of the Royal Society of New Zealand, 2020 - Taylor & Francis
ABSTRACT The 14th November 2016 Kaikōura earthquake was one of the most complex
crustal earthquakes recorded in the modern era. The rupture propagated northward for more …

Illuminating the pre‐, co‐, and post‐seismic phases of the 2016 M7. 8 Kaikōura earthquake with 10 years of seismicity

CJ Chamberlain, WB Frank, F Lanza… - Journal of …, 2021 - Wiley Online Library
Abstract The 2016 M7. 8 Kaikōura earthquake is one of the most complex earthquakes in
recorded history, with significant rupture of at least 21 crustal faults. Using a matched‐filter …

3D seismic velocity models for Alaska from joint tomographic inversion of body‐wave and surface‐wave data

A Nayak, D Eberhart‐Phillips… - Seismological …, 2020 - pubs.geoscienceworld.org
We present two new seismic velocity models for Alaska from joint inversions of body‐wave
and ambient‐noise‐derived surface‐wave data, using two different methods. Our work takes …

River patterns reveal two stages of landscape evolution at an oblique convergent margin, Marlborough Fault System, New Zealand

AR Duvall, SA Harbert, P Upton… - Earth Surface …, 2020 - esurf.copernicus.org
Here we examine the landscape of New Zealand's Marlborough Fault System (MFS), where
the Australian and Pacific plates obliquely collide, in order to study landscape evolution and …

Uplift and fault slip during the 2016 Kaikōura earthquake and late quaternary, Kaikōura Peninsula, New Zealand

A Nicol, J Begg, V Saltogianni… - New Zealand Journal …, 2023 - Taylor & Francis
ABSTRACT The Kaikōura Earthquake uplifted Kaikōura Peninsula by≤∼ 1 m. Uplift in 2016
mainly resulted from slip on an offshore thrust fault (OSTF), modelled to splay from the plate …

[HTML][HTML] Complex magmatic-tectonic interactions during the 2020 Makushin Volcano, Alaska, earthquake swarm

F Lanza, DC Roman, JA Power, CH Thurber… - Earth and Planetary …, 2022 - Elsevier
Abstract On June 15, 2020, at 21: 16 UTC, a locally-felt earthquake of magnitude 4.2 struck
Unalaska Island, Alaska,∼ 15 km west of the town of Unalaska and the large fishing port of …

Temporal relationship of slow slip events and microearthquake seismicity: Insights from earthquake automatic detections in the northern Hikurangi margin, Aotearoa …

J Yarce, AF Sheehan, S Roecker - Geochemistry, Geophysics …, 2023 - Wiley Online Library
Slow slip events in the northern Hikurangi margin of Aotearoa New Zealand occur every 18–
24 months and last for several weeks before returning to average convergence rates of …