[PDF][PDF] 南北地震带震源机制解与构造应力场特征

王晓山, 吕坚, 谢祖军, 龙锋, 赵小艳, 郑勇 - 地球物理学报, 2015 - dsjyj.com.cn
摘要南北地震带作为中国大陆地应力场一级分区的边界, 其构造应力场的研究对理解大陆强震
机理, 构造变形和地震应力的相互作用具有重要意义. 本文收集南北地震带1970—2014 …

Iterative joint inversion for stress and fault orientations from focal mechanisms

V Vavryčuk - Geophysical Journal International, 2014 - academic.oup.com
Stress inversions from focal mechanisms require knowledge of which nodal plane is the
fault. If such information is missing, and faults and auxiliary nodal planes are interchanged …

Episodic stress and fluid pressure cycling in subducting oceanic crust during slow slip

E Warren-Smith, B Fry, L Wallace, E Chon… - Nature …, 2019 - nature.com
Slow slip events are part of a spectrum of aseismic processes that relieve tectonic stress on
faults. Their spatial distribution in subduction zones has been linked to perturbations in fluid …

MSATSI: A MATLAB package for stress inversion combining solid classic methodology, a new simplified user‐handling, and a visualization tool

P Martínez‐Garzón, G Kwiatek… - Seismological …, 2014 - pubs.geoscienceworld.org
The estimation of the stress-field orientation from focal mechanisms of earthquakes is a
relevant tool to understand crustal mechanics and the physics of earthquakes. In global …

Calculating horizontal stress orientations with full or partial knowledge of the tectonic stress tensor

B Lund, J Townend - Geophysical Journal International, 2007 - academic.oup.com
Earthquakes potentially serve as abundant and cost-effective gauges of tectonic stress
provided that reliable means exist of extracting robust stress parameters. Several algorithms …

Retracing the Africa–Eurasia nascent convergent boundary in the Western Mediterranean based on earthquake and GNSS data

A Billi, M Cuffaro, B Orecchio, M Palano, D Presti… - Earth and Planetary …, 2023 - Elsevier
In the western Mediterranean, following the intervening continent-continent collision, the
subduction of the Tethyan ocean has progressively come to an end or almost in large …

Change in stress field after the 2011 great Tohoku-Oki earthquake

A Hasegawa, K Yoshida, Y Asano, T Okada… - Earth and Planetary …, 2012 - Elsevier
Temporal change in the stress field after the 2011 great Tohoku-Oki earthquake was
observed by using stress tensor inversions of earthquakes near the source region. In the …

Focal mechanisms and tectonic stress field in the North-South Seismic Belt of China

XS WANG, J LÜ, ZJ XIE, F LONG, XY ZHAO… - Chinese Journal of …, 2015 - en.dzkx.org
Abstract The North-South Seismic Belt is the boundary between the first-order blocks of the
tectonic stress field in China. The focal mechanisms of 819 events that occurred in this belt …

Three-dimensional variations in present-day tectonic stress along the Australia–Pacific plate boundary in New Zealand

J Townend, S Sherburn, R Arnold, C Boese… - Earth and Planetary …, 2012 - Elsevier
Using a newly compiled data set of 3424 focal mechanisms, we have estimated tectonic
stress parameters at 100 locations throughout central New Zealand in the largest study to …

[PDF][PDF] 汤加-克马德克俯冲带现今非均匀应力场特征及其动力学意义

黄骥超, 万永革, 盛书中, 李祥, 高熹微 - 地球物理学报, 2016 - researchgate.net
摘要汤加—克马德克俯冲带是太平洋板块向澳大利亚板块俯冲碰撞的动力作用区,
是全球俯冲带动力学研究的热点区域. 本研究基于EHB 地震目录, 对汤加—克马德克俯冲带(18.5 …