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662 results for “seismicity”
ARFM(Adaptive receiver function seismic migration): codes and dataset for application in SE Tibetan plateau
<p>We develop a post-stack adaptive receiver function (RF) seismic migration method to image subsurface disconitnuities. Contents of numerical experiments are in the compressed file 'program_synthetic_experiments.tar'. RF dataset and codes for the application of the adaptive receiver function migration method in southeastern Tibetan plateau are in other compressed files.</p>
Seismic study on lithosphere evolution for Mesozoic multiple stages gold deposits focusing in Southwestern China
<p>Dispersion files for ambient noise tomography, PRF file for P-wave receiver function and SRF file for S-wave receiver function</p>
Seismic modeling of a very young SPB star – KIC 8264293
<p>An inlists for MESA v9575, used to compute a grid of evolutionary models used in the paper "Seismic modeling of a very young SPB star – KIC 8264293".</p>
Seismically imaged mantle exhumation in the Southwest Taiwan Basin of the northeastern South China Sea margin
<p>Dataset for submission of Geochemistry, Geophysics, Geosystems.</p>
Original waveform of HAVESArray portable seismic network in Hainan Island and surrounding areas
<p>The waveform in this folder was recorded by the National Institute of Natural Hazards (NINH) (cut by catalog from 2018 and 2020). Waveform data were intercepted from the 20s before and 20s after the theoretical arrival-time of Pn. It is only used for scientific research.</p>
Coupled lithospheric deformation in the Qinling Orogen, central China: Insights from seismic reflection and surface-wave tomography
<p><strong>Data of geochronology of intrusive plutons and selected zircon Hf values shown in Figure S1 and the references cited</strong></p>
Seismic data for turbulence estimation 97306
<p>Water colunm reflection of seismic data 97306 acquired in 2001 in the northeastern South China Sea and Philippine Sea, acrossing the Luzon Strait.</p>
Seismic velocity models (Vp, Vs and Vp/Vs) of the Beaufort Sea continental margin
<p>This folder contains the local tomography software (LOTOS, Koulakov et al. 2009), three-dimensional seismic velocity models (Vp, Vs and Vp/Vs) and the earthquake relocations presented in "Seismic evidence for a weakened thick crust at the Beaufort Sea continental margin" submitted to <em>Geophysical Research Letters</em>. Please consult the detailed description of these files provided by I. Koulakov (http://www.ivan-art.com/science/LOTOS/).</p> <p>Koulakov, I. (2009). LOTOS code for local earthquake tomographic inversion: Benchmarks for testing tomographic algorithms. Bulletin of the Seismological Society of America, 99 (1), 194–214. doi: https://doi.org/10.1785/0120080013</p>
Seismic evidence on crustal architecture of east-southern Tibet and implications for active landform construction since Late Miocene
<p>This is the receiver function data set for "Seismic evidence on crustal architecture of east-southern Tibet and implications for active landform construction since Late Miocene"</p>
dataset used in article entitiled "Heterogeneous shear strength around mainshock fault of the 2000 Western Tottori earthquake (M 7.3) through dense seismic observations"
<p>See README.doc for description about the files.</p>
the dataset for "Investigating multiple observations around a seismic gap during the Lushan earthquake in Sichuan, China"
<p>The relocation of the earthquake before and after Lushan earthquakes.</p>
A lower mantle slab below the East Asia margin constrained by seismic waveform complexity
<p>This dataset consists of two parts: the waveforms of four events and the calculated MPD data for three of them. The waveforms for each event are recorded at the stations along the 2D profile. While the MPD data contains all the stations from the China National Seismic Network. </p>
Data and program codes to reproduce the results of seismic tomography for La Palma Island
<p>This file contains the files to reproduce the results presented in the article: <strong>Voluminous storage and rapid magma ascent beneath La Palma revealed by seismic tomography </strong>by Luca D'Auria, Ivan Koulakov, Janire Prudencio, Iván Cabrera-Pérez, Jesús M. Ibáñez, Jose Barrancos, Rubén García-Hernández, David Martínez van Dorth, Germán D. Padilla, Monika Przeor, Victor Ortega, Pedro Hernández, Nemesio M. Peréz, <em>Scientific Reports</em>.</p> <p>This file includes:</p> <p>1. The full folder with the LOTOS code for the passive-source seismic tomography (Koulakov, 2009, BSSA). </p> <p>2. Folder with the dataset including arrival times of the P and S waves from local seismicity in the area of the La Palma Island, Canary Archipelago.</p> <p>3. README_LA_PALMA.PDF file with the description of the workflow on how to reproduce the tomography models based on experimental and synthetic data presented in the article. </p> <p>Koulakov, I., 2009, LOTOS code for local earthquake tomographic inversion: Benchmarks for testing tomographic algorithms: Bulletin of the Seismological Society of America, v. 99, p. 194–214, https://doi.org/10.1785/0120080013.</p>
Seismic homogenization of poroelastic regions in absence of a representative elementary volume
<p>Data used for figures. Read the list_files.txt to find the corresponding files.</p>
The datasets for the paper "Spatial and temporal distribution of lobate scarps in the lunar south polar region: Evidence for latitudinal variation of scarp geometry, kinematics and formation ages, continuous tectonic activity in the last 100 million years and seismically safe south pole Artemis human landing site" Geophysical Research Letters.
<p>This dataset provides the original data that were used for preparing the illustrations, figures and tables.</p>
Physiological responses of narwhals to anthropogenic noise: a case study with seismic airguns and vessel traffic in the Arctic
<p>Limited polar geographical range, narrowly defined migratory routes, and deep-diving behaviors make narwhals exceptionally vulnerable to anthropogenic disturbances including oceanic noise. Although behavioral studies indicate marked responses of cetaceans to disturbance, the link between fear reactions and possible injury from noise exposure is limited for most species.</p> <p>To address this, we deployed custom-made heart rate-accelerometer-depth recorders on 13 adult narwhals in Scoresby Sound, East Greenland across a five-year period (2014-2018). Physiological responses of the cetaceans were monitored in the absence (n = 13 animals) or presence (n = 2 animals across 3 acoustic events) of experimentally directed, seismic airgun pulses and associated vessels (full volume source level = 241 dB re 1 μPa-m).</p> <p>We found that anthropogenic noise resulted in marked cardiovascular, respiratory and locomotor reactions by two narwhals exposed to seismic pulses across three acoustic events. The general behavioral response to seismic and vessel noise included an 80% reduction in the duration of gliding during dive descents by seismic-exposed narwhals compared to controls, and the prolongation of high-intensity activity (ODBA > 0.20 g) with elevated stroke frequencies exceeding 40 strokes per minute. Noise exposure also resulted intense (< 10 bpm) bradycardia that was decoupled from stroking frequency. This decoupling instigated increased variability in heart rate, with the heart switching rapidly between bradycardia and exercise tachycardia during noise exposure. Maximum respiratory frequency following seismic exposure, 12 breaths.min<sup>-1</sup>, was 1.5 times control levels.</p> <p>Overall, the effect of seismic/ship noise exposure on wild narwhals was a 2.0 – 2.2-fold increase in the energetic cost of diving, which paradoxically occurred during suppression of the cardiac exercise response. This unusual relationship between diving heart rate and exercise intensity represents a new metric for characterizing the level of fear reactions of wild marine mammals exposed to different environmental stressors. Together, the multi-level reactions to anthropogenic noise by this deep-diving cetacean demonstrated how a cascade of effects along the entire oxygen pathway could challenge physiological homeostasis especially if disturbance is prolonged.</p>
Hu et al., 'The productivity of induced seismicity is controlled by injection fluid volume and preexisting faults in southern Sichuan Basin'
<p>1. Earthquake catalog:Earthquake catalogs within 2 kilometers of each platform (N5 and N7). The 10 columns from left to right are year, month, day, hour, minute, second, latitude, longitude, depth and magnitude.</p> <p>2. Injection Volume of all wells:Fracturing injection volume per stage per horizontal well. The 4 columns from left to right are Serial number of well & pads, Fracturing section number, Fracturing time span and Total injection volume (m3).</p> <p>3. The range of Spatiotemporal Association Filter (SAF):SAF vertex coordinates for six individual fracture well groups. The first column is the boundary of horizontal well trajectory and the boundary of Spatiotemporal Association Filter (SAF) from top to bottom. The second column is the names of the four vertices. Columns 3 through 12 show longitude and latitude for each well group, respectively.</p> <p>4. Waveform Data:Waveforms of the selected earthquakes with focal mechanism solutions.</p>
Seismic ambient noise CCFs at Suwanosejima volcano, Japan
<p>The dailyCCF.tar contains data of daily seismic ambient noise CCFs at Suwanosejima volcano, Japan (April 1, 2017-December 31, 2021). These CCFs have been used to create the results in the accompanying paper "Seismic scattering property changes correlate with ground deformation at Suwanosejima volcano, Japan" by Takashi Hirose, Hideki Ueda, and Eisuke Fujita, submitted to the Journal of Geophysical Research: Solid Earth (https://doi.org/10.1002/essoar.10510785.2).</p>
Seismic catalogue Campi Flegrei 1982-1984
<p>This is a temporary database, an updated database will be created within the INGV database </p>
Tilt and seismic data of Stromboli volcano, Italy
<p>Tilt and seismic data of Stromboli volcano, Italy, in MATLAB binary files (.mat).</p> <p>/2014/ - Three temporary tilt stations (CPL, PZZ, RFR) and three permanent til stations (OHO, LFS, LSC) from1 June to 18 August 2014.</p> <p>/2019/ - Five permanent seismic stations (SCI, ROC, STR, PZZ, SDK) and one permanent tilt station (OHO) from1 to 3 July 2019.</p>
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International Brain Laboratory public data
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OpenNeuro
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