Article
Geochemistry & Geophysics
Osamu Sandanbata, Hiroo Kanamori, Luis Rivera, Zhongwen Zhan, Shingo Watada, Kenji Satake
Summary: The method of estimating ring-fault parameters based on MT solutions obtained from long-period seismic records is proven to be effective, enabling the examination of the kinematics and structures below active volcanoes with ring faults globally.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geosciences, Multidisciplinary
David R. R. Shelly, Robert J. J. Skoumal, Jeanne L. L. Hardebeck
Summary: In August 2020, a seismic sequence began in the Maacama fault zone in northern California, leading to questions about its connection with a larger fault. Through various seismic analysis techniques, including event detection, relocation, and focal mechanisms, the researchers investigated the faulting geometry and its impact on seismic activity. They discovered that the sequence originated from a right-lateral fault, likely a section of the Maacama Fault, but also activated numerous left-lateral conjugate faults, forming a fracture mesh consistent with fluid-induced faulting and earthquake swarms seen elsewhere.
GEOPHYSICAL RESEARCH LETTERS
(2023)
Article
Geochemistry & Geophysics
Yu Jiang, Sergey V. Samsonov, Pablo J. Gonzalez
Summary: Improved imaging of fault slip is crucial for understanding earthquakes and faulting. By introducing a new regularization method, we successfully recovered complex slip propagation patterns and estimated the spatio-temporal evolution of fault slip. Applying the method to a seismic swarm, we found that aseismic slip played a significant role and the slip rates were consistent with slow earthquake processes.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2022)
Article
Geochemistry & Geophysics
Mohammad Reza Sheikholeslami, Parisa Mobayen, Hamid Reza Javadi, Mohammad R. Ghassemi
Summary: This paper presents the latest data on the stress pattern and tectonic regime in Central Iran, based on focal mechanism data collected from GCMT, HRVD, and ISC. The study reveals a dominant N029 degrees E maximum horizontal compressive stress direction in the region, indicating a general compressive tectonic regime.
Article
Environmental Sciences
Davide Zaccagnino, Carlo Doglioni
Summary: This study found that earthquakes on thrust faults have a higher double couple component compared to earthquakes on strike-slip and normal faults, which may be due to the more mature fault zone structure. This finding has important implications for seismic forecasting and magnitude estimation.
COMMUNICATIONS EARTH & ENVIRONMENT
(2022)
Article
Geosciences, Multidisciplinary
Violeta Veliz-Borel, Vasiliki Mouslopoulou, Andrew Nicol, John Begg, Onno Oncken
Summary: This study focuses on the upper-plate normal faults along the forearc of the Hellenic Subduction System (HSS) in Greece. Detailed field-mapping and analysis of high-resolution Digital Elevation Models (DEMs) were used to study active normal faults on Kythira and Antikythira islands. The results show that these faults have different lengths and scarp heights, accommodating trench-orthogonal extension during the Quaternary. Rate variability between different time intervals and across the entire fault network suggests earthquake clustering may occur over relatively short timescales.
FRONTIERS IN EARTH SCIENCE
(2022)
Article
Geochemistry & Geophysics
Wenhuan Kuang, Congcong Yuan, Jie Zhang, Wei Zhang
Summary: Earthquake focal mechanisms are important for understanding faulting geometry and stress distributions. Existing approaches are limited by uncertainties in velocity models. This study proposes a relative focal mechanism inversion method that utilizes a well-constrained primary event. Testing on synthetic and real earthquake data demonstrates the robustness and improved consistency of the proposed method. It provides reliable earthquake focal mechanisms for the investigation of the earthquake process.
SEISMOLOGICAL RESEARCH LETTERS
(2023)
Article
Geosciences, Multidisciplinary
Jidong Yang, Hejun Zhu, Thorne Lay, Yufeng Niu, Lingling Ye, Zhong Lu, Bingxu Luo, Hiroo Kanamori, Jianping Huang, Zhenchun Li
Summary: The earthquake near Stanley, Idaho in March 2020 was caused by a complex source, involving a pair of opposing-dip faults with strike-slip and normal faulting. The converging fault geometry allowed the rupture to traverse a 10-km-wide step, which is uncommon in earthquake ruptures. This study provides insights into the rupture process of earthquakes near the northern boundary of the Centennial Tectonic Belt.
GEOPHYSICAL RESEARCH LETTERS
(2021)
Article
Geochemistry & Geophysics
Osamu Sandanbata, Shingo Watada, Kenji Satake, Hiroo Kanamori, Luis Rivera, Zhongwen Zhan
Summary: The main cause of tsunamis is large subduction zone earthquakes, but submarine volcanic processes can also generate tsunamis. This study used tsunami and seismic data from the 2015 event to show that the uplift of a submarine caldera due to overpressure in its magma reservoir caused an earthquake and tsunami. The mechanism of tsunami generation by submarine trapdoor faulting highlights the importance of monitoring submarine calderas for accurate assessment of tsunami hazards.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2022)
Article
Engineering, Geological
Kunbo Wu, Junpeng Zou, Yu-Yong Jiao, Xiufeng Zhang, Chao Wang
Summary: Strong seisms triggered during deep coal mining pose a serious threat to the safety of underground miners and ground residents. Investigating focal mechanisms and source parameters of seisms is essential for understanding rock fracturing and rupture scale. However, such research is lacking in deep mines. This study analyzed over 11,000 seismic events in Dongtan Coal Mine and proposed a new criterion for determining rock fracture type. The formation mechanisms of strong seisms in mines were categorized and the correlation of source parameters was revealed.
ROCK MECHANICS AND ROCK ENGINEERING
(2023)
Article
Geochemistry & Geophysics
A. I. Filippova, V. I. Melnikova
Summary: The East Arctic region is crucial for understanding the geodynamic pattern and lithospheric evolution of the entire Arctic. In order to fill the gap in regional seismic data, source parameters for 103 earthquakes (Mw=4.2, 1990-2021) were calculated and a representative uniform data set was compiled. The results reveal dominant extension along the Gakkel Ridge and Laptev Sea shelf, with compression replacing it on the continent and east and west of the shelf. The spreading axis of the Gakkel Ridge does not continue to the Laptev Sea shelf, and evidence for the Eurasian-North American plate boundary crosses the eastern Laptev Sea shelf and is likely to pass through the Yana Bay to the Chersky Range.
Article
Geochemistry & Geophysics
Ahad Nouri, Behnam Rahimi, Vaclav Vavrycuk, Farzin Ghaemi
Summary: We analyzed the stress field in the Zagros fold-and-thrust belt (ZFTB) by studying 898 mainshock focal mechanisms between 1956 and 2021. The results showed heterogeneous crustal stress with variations in SHmax orientation and stress ratio. The study identified three distinct domains (northern, central, and southern) with different tectonic regimes (wrench, compressional, and wrench-compressional to compressional). Convergence between the Arabian and Iranian plates was determined as the primary factor influencing deformation and seismicity in the ZFTB zone.
Article
Geology
Nadine G. Reitman, Yann Klinger, Richard W. Briggs, Ryan D. Gold
Summary: This study examines the influence of climate on the decay rate of large offsets in earthquake fault systems. The findings reveal that high mean annual precipitation is associated with a slower decay rate of large offsets. This suggests that climate plays a significant role in the development and preservation of offset channels.
Article
Geosciences, Multidisciplinary
Chi-Hsien Tang, Ya-Ju Hsu, Teresito Bacolcol, Yunung Nina Lin, Horng-Yue Chen, Yu-Ting Kuo, Hsuan-Han Su, Hsin-Ming Lee, Alfie Pelicano, Genesis Sapla, Shui-Beih Yu
Summary: On July 27, 2022, a magnitude 7.0 Abra earthquake struck northwestern Luzon, Philippines, causing 11 deaths, damaging over 30,000 buildings, and resulting in $34 million worth of damage. The earthquake occurred on a previously unrecognized deep fault with no observable surface ruptures. Using data from the Global Navigation Satellite System and Interferometric Synthetic Aperture Radar, researchers were able to investigate the source fault and distribution of coseismic slip. The study revealed that the coseismic slip occurred beneath the Philippine Fault Zone in northern Luzon at a depth of 11-22 km.
GEOPHYSICAL RESEARCH LETTERS
(2023)
Article
Geochemistry & Geophysics
Susumu Shibutani, Weiren Lin, Koichiro Sado, Akihiro Aizawa, Katsuaki Koike
Summary: This study reveals the fault characteristics and surrounding lithological units of the 2016 Kumamoto earthquake mainshock triggered by the Futagawa fault through a multiple-borehole drilling. It is found that there is more than 200 meters of normal faulting displacement along the Futagawa fault, and the 461 damage zone is identified as the primary candidate for the seismogenic faulting during the earthquake.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2022)