High-rate GNSS has been proven effective in characterising waveforms and co-seismic displacements due to medium-to-strong natural earthquakes. No application focused on small magnitude events like shallow anthropogenic earthquakes, where displacements and noise have the same order of magnitude. We propose a procedure based on proper signal detection and filtering of the position and velocity time series obtained from high-rate (10 Hz) GNSS data processing with two intrinsically different approaches (Precise Point Positioning and variometry). We tested it on five mining tremors with magnitudes of 3.4-4.0, looking both at event detection and its kinematic characterisation. Here we show a high agreement, at the level of 1 s, between GNSS and seismic solutions for the earthquake first epoch detection. Also, we show that high-rate multi-constellation (GPS + Galileo) GNSS can reliably characterise low-magnitude shallow earthquakes in terms of induced displacements and velocities, and, including their peak values, respectively, at the level of very few millimetres and 1-2 cm/s, paving the way to the routine use of GNSS-seismology for monitoring human activities prone to cause small earthquakes and related potential damages.
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http://dx.doi.org/10.1038/s41598-023-47964-2 | DOI Listing |
Proc Natl Acad Sci U S A
January 2025
Department of Civil and Environmental Engineering, Western University, London, ON N6A 5B9, Canada.
Induced earthquakes are manifestations of highly heterogeneous distributions of effective stress changes imparted by anthropogenic activities such as hydraulic fracturing and wastewater injection. It is critical to disentangle the mechanisms behind these earthquakes to better assess seismic risk. Here, a clustering methodology is applied to a catalog of 21,536 induced earthquakes detected during a 36-d hydraulic stimulation program in Western Canada.
View Article and Find Full Text PDFTurbidity flows can transport massive amounts of sediment across large distances with dramatic, long-lasting impacts on deep-sea benthic communities. The 2016 M 7.8 Kaikōura Earthquake triggered a canyon-flushing event in Kaikōura Canyon, New Zealand, which included significant submarine mass wasting, debris, and turbidity flows.
View Article and Find Full Text PDFPLoS One
December 2024
Department of Invertebrate Zoology, Institute for Biodiversity Science and Sustainability, California Academy of Sciences, San Francisco, California, United States of America.
In the aftermath of the 2011 east Japanese earthquake and tsunami, anthropogenic debris from the east coast of Japan floated across the Pacific Ocean to the west coast of North America. One such vessel from Iwate Prefecture arrived on the coast of Oregon, and the fouling community included specimens identified as the nudibranch Hermissenda crassicornis, which was previously thought to range from Japan to Baja California but has since been split into three species: H. crassicornis (northeastern Pacific), H.
View Article and Find Full Text PDFEnviron Sci Pollut Res Int
December 2024
Department of Geography, Institute of Science, Banaras Hindu University, Uttar Pradesh, Varanasi, 221005, India.
The mountainous region, which holds a diverse ecosystem providing services of global importance, is fragile owing to the varied topography and continuous human pressure. The risk from natural hazards in mountainous regions is substantial posing significant challenges and causing causalities. Northwestern Himalayas being located in the junction of the Eurasian and Indo-Australian plates are delicate and face the brunt of vagaries from multiple hazards as well as anthropogenic pressure.
View Article and Find Full Text PDFEnviron Sci Pollut Res Int
August 2024
Dipartimento Di Ingegneria, Università Degli Studi Di Napoli Parthenope, 80133, Naples, Italy.
Conventional geodetic methods rely on point measurements, which have drawbacks for detecting and tracking geologic disasters at specific locations. In this study, the time series Interferometric Synthetic Aperture Radar (InSAR) approach was incorporated to estimate non-linear surface deformation caused by tectonic, shoreline reclamation, and other anthropogenic activities in economically important urban regions of Pakistan's southern coast, which possesses around 270 km. The shoreline is extended from the low-populated area on the premises of the Hub River in the west to the highly populated Karachi City and Eastern Industrial Zone, where we collected the Sentinel-1A C-band data from 2017 to 2023 to address urban security and threats to human life and property.
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