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562 results for “Faults”
The effect of shear strain and shear localization on fault healing
<p>This is the ReadMe file corresponding to the study entitled:<br> "The effect of shear strain and shear localization on fault healing"<br> By Noël C., Giorgetti C., Collettini C. and Marone C.</p> <p>This Read-Me file has been last edited in August 2023</p> <p>This readme file describes the data repository and supplementary files accompanying the above publication. <br> For any further queries please contact corentin.noel@geoazur.unice.fr</p>
The Geodetic Signature of Bookshelf Faulting in Nicaragua
<p>GPS time series plots and Boundary Element model inputs for 3D-Def software for models presented in study.</p>
Ceraunius Fossae and Tractus Fossae, Mars, Fault Catalogue
<p>Catalogue of all faults in Ceraunius Fossae and Tractus Fossae, Mars, in shapefile format. Faults are mapped on Context Camera (CTX) images, within the Tanaka et al. (2014) unit boundary outlines.</p>
Ramp-Flat and Splay Faulting Illuminated by Frictional Afterslip Following the 2017 Mw 7.3 Sarpol-e Zahab Earthquake
<p>The postseismic InSAR data used in the manuscript "Frictional Afterslip along a Complex Fault Structure Following the 2017 Mw 7.3 Sarpol-e Zahab Earthquake Revealed by InSAR and 2-D Finite Element Models".</p>
Parallel window decoding enables scalable fault tolerant quantum computation
<p>Dataset containing raw data presented in the publication <em>"Parallel window decoding enables scalable fault tolerant quantum computation"</em> as well as the stim circuits used to sample circuit-level noise.</p> <p> </p>
Lithospheric structure controls the sequentially active detachment faulting at the Longqi segment on the Southwest Indian Ridge
<p><strong>supplementary materials for "Lithospheric structure controls the sequentially active detachment faulting at the Longqi segment on the Southwest Indian Ridge"</strong></p>
Data from: Crustal faulting drives biological redox cycling in the deep subsurface
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Strain localization in sandstone-derived fault gouges under conditions relevant to earthquake nucleation
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Three-dimensional offsets of geomorphic piercing lines displaced by the quaternary-active Beaufort range fault, northern Cascadia forearc, BC, Canada
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Data for paper: Control of fault weakening on the structural styles of underthrusting-dominated non-cohesive accretionary wedges
<p>This repository contains data related to the paper:<br> A. Bauville, M. Furuchi and M. Gerbault, Control of fault weakening on the structural styles of underthrusting-dominated non-cohesive accretionary wedges, Journal of Geophysical Research, 2020.</p> <p>It contains data for all simulations shown in Fig. 7 (last timestep)</p> <p>List of file for each simulations:<br> modelState.json: json file containing various information about the state of the model<br> particles_strain.bin: binary file containing strain data for all particles<br> particles_x.bin: current x position for all particles<br> particles_y.bin: current y position for all particles<br> particles_xIni.bin: initial x position for all particles<br> particles_yIni.bin: initial y position for all particles</p> <p># File format<br> n, u, data</p> <p>n = number of particles bytesize=[1 * int32]<br> u = characteristic unit bytesize=[1 * double]<br> data = data for n particles bytesize=[n * single]</p> <p># example to extract data from bin files in python<br> import numpy as np<br> import os</p> <p>with open(FileName, 'rb') as f:<br> f.seek(12, os.SEEK_SET)<br> data = np.fromfile(f, dtype=np.single, count=-1, sep='')</p>
Data set to ''Volcano growth versus deformation by strike-slip faults: morphometric characterization through analogue modelling'
<p>This data set is the supplementary material to Grosse et al. (2020) 'Volcano growth versus deformation by strike-slip faults: morphometric characterization through analogue modelling', published in Tectonophysics (https://doi.org/10.1016/j.tecto.2020.228411). The data set consists of (1) 249 digital elevation models (DEMs) of each step of the the analogue experiments carried out, in standard ENVI format, zipped; and (2) an Excel file containing the DEM-derived morphometric parameters for each of the analogue models.</p> <p>Experiments were carried out at the analogue modelling lab of the Department of Geography at the Vrije Universiteit Brussel (Belgium). A granular mixture of fine-grained quartz sand and kaolin clay was used as analogue material. Experiments were conducted on a fixed table, on which a basal layer of granular material was placed. A basal plate attached to a step-motor was used to simulate pure strike-slip displacements of the basal layer. Volcano growth was simulated by depositing loads of granular material on top of the basal layer from a point source. The analogue models were photographed at regular time intervals during the experiments using four digital cameras. The photographs were used to generate synthetic digital elevation models (DEMs) with 0.2 mm spatial resolution of each step of the analogue models by applying the MICMAC digital stereo-photogrammetry software. The ENVI software was used to re-sample the DEMs to a 0.5 mm spatial resolution and apply the noise-reduction Lee filter. Morphometric data were then extracted from the DEMs by applying two IDL-language algorithms: NETVOLC, used to automatically calculate the volcano edifice basal outline, and MORVOLC, used to extract a set of morphometric parameters.</p>
DATA SET FOR: Active faulting, submarine surface rupture and seismic migration along the Liquiñe-Ofqui fault system, Patagonian Andes
<p>Data description: These data corresponde to high-resolution bathymetry and seismic reflection profiles obtained in the inner fjord west of Puerto Aysén (between 73.13°- 72.68°W and 45.32°-45.47°S; Figs. 1 and 2). The data set was obtained during a geophysical study as part of the DETSUFA project (Deslizamientos Tsunamigénicos en el Fiordo de Aysén; Lastras et al., 2013), which took place between March 4th and 17th, 2013, aboard the R/V BIO Hésperides.<br> <br> KONGSBERG SIMRAD multibeam EM-1002S was used to obtain bathymetric data, and it works with 111 beams at a 96 kHz sonar frequency and with a maximum ping rate of >10 Hz. Equidistant mode was used for swath bathymetry acquisition. This array maximized the number of beams facilitating data acquisition and obtaining a homogenized final grid with improved resolution, with tracks separated every 150 m. The swath thickness was the same regardless of width, generating a 50% overlap between each track, with the exception of areas located near the coast. Expendable Bathythermograph (XBT) probes were used at specific sites to measure changes in water sound velocity due to eventual changes in fresh water circulation, tides, and sediment.<br> <br> Seismic reflection data were acquired using an array of two BOLT air guns (165 and 175 inches3), which were towed behind the vessel stern. The configuration used in the seismic sources was 2,000 psi, a depth of 3 m for the gun, with a firing rate of 15 m over the seafloor. A 100 m long mini-streamer with a 25 m active section, corresponding to one single channel, recovered the shots. The seismic data were recorded by using the DELPH SEISMICPLUS system with a recording length of 4.0 s and a preamplifier gain of 8 Hz. The raw seismic data were processed aboard the SMT Kingdom Suite, including the navigation and standard processes of electrical noise removing (50 Hz filter), gain amplifier and bandpass filtering, to improve data visualization. Postprocessing included the migration of the sea bottom diffractions and the muting of the water column performed in Seismic-Unix.</p> <p>Files:</p> <p>Raw Seismic reflection data for lines 05, 06 and 07 (SU & SEG files)</p> <p>Masked Seismic profiles for lines 05, 06 and 07 (SU, PDF & PS files)</p> <p>Bathymetry of inner and outer Aysén Fjord (ASCII file)</p>
Data for: Historical earthquake scenarios for the middle strand of the North Anatolian Fault deduced from archeo-damage inventory and building deformation modeling
<p>This dataset is associated to the article "Historical earthquake scenarios for the middle strand of the North Anatolian Fault deduced from archeo-damage inventory and building deformation modeling " published in Seismological Research Letters (<a href="https://pubs.geoscienceworld.org/ssa/srl/article-abstract/doi/10.1785/0220200278/592607/Historical-Earthquake-Scenarios-for-the-Middle?">link</a>).</p> <p>It includes the following:</p> <ul> <li>The annotated photographs of the EAE (Earthquake Archeological Effects) inventoried in Iznik ("EAE_xxx.pdf").</li> <li>The 3D displacement signals used as input for obelisk modeling ("Displacement_xxx").</li> <li>The output obelisk displacement curves and final block shift values relative to base ("Obelisk_block_motion.pdf").</li> </ul>
Displacement accumulation and sampling of paleoearthquakes on active normal faults of Crete in the eastern Mediterranean
<p>The Table S1 (uploaded separately) presents fault data and calculated values of earthquake parameters that underpin the interpretations and conclusions presented in Nicol et al. (G3, submitted June 20, 2020). The Locations of each fault are shown in Figure 2 of the main manuscript.</p> <p>In detail: The Table S1 summarises the attributes on all active faults studied on Crete. Single Event Displacement (SED), Recurrence Interval (RI), Moment Magnitude (M<sub>w</sub>) and number of paeoearthquakes have been estimated for each fault using topographic fault lengths and Quaternary displacement rates in conjunction with the Wesnousky (2008) equations (see table footnote for equations used to calculate SED and Mw). Mw calculated using Wesnously (2008) equations are unconstrained at lengths < 15.5 km. Note that the short-term (e.g. the post-glacial period) displacement rates for the Lentas (ID=43) and South Central Crete (ID=44) faults derive from time periods of c. 50 kyr and 125 kyr, respectively (from Gallen et al., 2014). Nevertheless, the estimated number of events on these two faults correspond to the post-glacial period (16.5 kyr). Table S1 presents uncertainties of +40% and -20% for maximum displacements derived from topography. Here we are conservative and have allowed larger errors for the maximum fault displacements to account for greater errors associated with erosion. The calculated earthquake recurrence interval (RI) in Table S1 derives from SED/Quaternary displacement rate.</p>
The 2009 Mw6.1 L'Aquila normal fault system imaged by 64,051 high-precision foreshock and aftershock locations.
<p>The earthquake catalogue is composed by 64,051 high-precision foreshock and aftershock recorded during the Mw6.1 2009 L'Aquila (Central Italy) normal faulting seismic sequence. The catalog includes events occurred between 1<sup>st</sup> of January and 31<sup>st</sup> December 2009. The completeness magnitude is 0.7. Earthquake locations were obtained by combining an automatic picking procedure for P and S waves, together with cross-correlation and double-difference location methods. </p> <p>Seismic data were recorded at a very dense local network composed of 67 three-component seismic stations (20 permanent stations of the Italian National Network located within 80 km from the epicentral area and 47 temporary stations installed soon after the occurrence of the main shock [Margheriti et al., 2011]). </p> <p>Earthquakes were extracted by the continuous recordings by applying a detection algorithm to all stations, based on the classical STA/LTA coincidence-sum algorithm applied to the trace of the 3C covariance matrix. To these events, we applied an automatic picking algorithm (Manneken Pix) [Di Stefano et al., 2006] able to provide about 1.9 million P-wave and 503,000 S-wave accurate readings, with an estimation of the measurement errors. </p> <p>We applied a time domain cross-correlation method (Schaff and Waldhauser, 2005) to all event pairs with separation distances ≤ 5 km at all stations that recorded the pair. Seismograms were filtered in the 1-15 Hz frequency range using a 4 pole, zero phase band‐pass Butterworth filter. We selected measurements with correlation coefficients greater than 0.85, resulting in a total of ~190 million P and ~85 million S-wave delay times. </p> <p>Earthquakes were located following a two steps procedure. Initial locations for 133,236 events were computed with the Hypoellipse code [Lahr , 1989] using a 1D P-wave gradient velocity model optimized for the area [Chiaraluce et al., 2011]. In the second step, we computed relative locations by applying the large scale double-difference method described in Waldhauser and Schaff, (2008) to the catalog picks and phase delay times measured from waveform cross correlation. The entire dataset was sub-divided in 84 rectangular overlapping boxes, containing a maximum of 3000 earthquakes, orthogonal to the mean strike of the seismic sequence. Resulting relative locations from all boxes were combined into a single catalog, computing the weighted mean of double hypocenters in the overlapping regions (Waldhauser and Schaff, 2008). </p> <p>The final double-difference catalog includes 64,051 events. A subset made of 51,271 earthquakes (i.e., 80% of the whole dataset) indicates highly correlated earthquakes, having at least 10 P-waves and 5 S-waves correlated phases with at least one other event. Highly correlated events (flag=1 in the attached file) mostly occur on the major fault segments, while poorly correlated earthquakes (flag=0 in the attached file) mostly occur in the volume around the major faults.</p> <p>The attached file is a plain text with ";" separator and .csv extension.</p> <p>Here below the header is explained.</p> <p><strong>id_dd: </strong>the hypoDD unique event identifier</p> <p><strong>origin_time: </strong>date of the origin time in the format YYYY-MM-DD[T]hh:mm:ss.msec</p> <p><strong>lat</strong>: hypocenter latitude expressed in degrees </p> <p><strong>lon</strong>: hypocenter longitude east of Greenwich, expressed in degrees</p> <p><strong>dep</strong>: hypocenter depth expressed in km </p> <p><strong>mag</strong>: magnitude (pure number)</p> <p><strong>flag</strong>:<strong> </strong>1 for highly correlated earthquakes; 0 for poorly correlated earthquakes. </p> <p> </p> <p> </p> <p> </p>
Seismic datasets in "Conjugate fault deformation revealed by aftershocks of the 2013 Mw6.6 Lushan earthquake and seismic anisotropy tomography"
<p>The Lushan seismic dataset used in the manuscript entitled 'Conjugate fault deformation revealed by aftershocks of the 2013 Mw6.6 Lushan earthquake and seismic anisotropy tomography ' submitted to Geophysical Research Letters.</p> <p> </p>
Supporting Material to "Statistical Fault Attacks on Nonce-Based Authenticated Encryption Schemes"
<p>supporting_material_code/setX/ct_fault.txt: each line corresponds to one ciphertext received from the device under test while encrypting a plaintext. The bytes are separated by a comma. For every encryption a fault has been injected:</p> <p>set1: Laser fault injections targeting an AES co-processor on a smartcard microcontroller.</p> <p>set2: Clock tampering targeting an AES co-processor implemented on a general-purpose microcontroller.</p> <p>set3 & 4: Clock tampering targeting an AES software implementation (AVR crypto lib ASM) implemented on a general-purpose microcontroller (ATXmega256A3).</p> <p>supporting_material_code/main.cpp: program for key recovery which takes as input the faulty ciphertexts (ct_fault.txt)</p> <p> </p>
Apollo - List of Faults
<p>Overview of Data</p> <p>Bug Reports obtained from tool Apollo, used to find faults in PHP programs. The programs tested are faqforge, webchess, schoolmate, phpsysinfo</p> <p>Paper Abstract</p> <p>Web script crashes and malformed dynamically-generated Web pages are common errors, and they seriously impact usability of Web applications. Current tools for Web-page validation cannot handle the dynamically-generated pages that are ubiquitous on today’s Internet. In this work, we apply a dynamic test generation technique, based on combined concrete and symbolic execution, to the domain of dynamic Web applications. The technique generates tests automatically, uses the tests to detect failures, and minimizes the conditions on the inputs exposing each failure, so that the resulting bug reports are small and useful in finding and fixing the underlying faults. Our tool Apollo implements the technique for PHP. Apollo generates test inputs for the Web application, monitors the application for crashes, and validates that the output conforms to the HTML specification. This paper presents Apollo’s algorithms and implementation, and an experimental evaluation that revealed 214 faults in 4 PHP Web applications.</p> <p> </p>
Strain and slip data for Kinematic inversion of fault slip during the nucleation of laboratory earthquakes
<p>The file contains the timeseries of strain and average slip obatined from a 8 gauges array used to monitor an injection experiment on a saw-cut centimetric scale sample loaded in a triaxial cell, under 30 MPa, 60 MPa and 90 MPa of confining stress.</p>
Fluvial Response to Differential Activity of the Litang Fault System: Implications for Fault Kinematics and Geodynamics in the Southeastern Tibetan Plateau
<p>Supporting information accompanies the publication "Fluvial Response to Differential Activity of the Litang Fault System: Implications for Fault Kinematics and Geodynamics in Southeastern Tibetan Plateau ". </p> <p>Table S1 presents information related to all the extracted river channels including the drainage area and outlet elevation. The elevation, horizontal and vertical migration distances of knickpoints, as well as<em> ksn</em> values above and below the knickpoints have also been included.</p> <p>All the river longitudinal profiles extracted in this study, including the knickpoint position on the longitudinal profiles and the high-precision DEM data presented in Figures 9a and 10a, are provided .</p>
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