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203 results for “Seismic data”
Training, Validation and Test Sets for paper 'A Little Data goes a Long Way: Automating Seismic Phase Arrival Picking at Nabro Volcano with Transfer Learning'
<p>Training, Validation and Test Data for model presented in paper 'A Little Data Goes A Long Way: Automating Seismic Phase Arrival Picking at Nabro Volcano with Transfer Learning', submitted to Journal of Geophysical Research: Solid Earth.</p> <p>Files:</p> <p>- train_events_2498.h5 = training set of seismic waveforms (events with P-/S-wave labelled arrivals only, i.e., no noise waveforms)</p> <p>- train_events_2498.pkl = event training set metadata (UTC P-/S-wave phase arrival times)</p> <p>- train_noise_2498.h5 = training set of seismic waveforms (noise sections only, i.e., no event waveforms)</p> <p>- train_noise_2498.pkl = noise training set metadata (UTC time for training noise waveforms)</p> <p>- val_events.h5 = validation set of seismic waveforms (events with P-/S-wave labelled arrivals only, i.e., no noise waveforms)</p> <p>- val_events.pkl = event validation set metadata (UTC P-/S-wave phase arrival times)</p> <p>- val_noise.h5 = validation set of seismic waveforms (noise sections only, i.e., no event waveforms)</p> <p>- val_noise.pkl = noise validation set metadata (UTC time for validation noise waveforms)</p> <p>- test.h5 = test set of seismic waveforms (events and noise)</p> <p>- test_events.pkl = event test set metadata (UTC P-/S-wave phase arrival times for test event waveforms)</p> <p>- test_noise.pkl = noise test set metadata (UTC time for test noise waveforms)</p> <p>- nabro_2011-247.mseed = 24 hours seismic data from Nabro Urgency Array (2011-09-04), saved in mseed format (e.g., can be read with obspy)</p> <p>- nabro_2011-269.mseed = 24 hours seismic data from Nabro Urgency Array (2011-09-26), saved in mseed format (e.g., can be read with obspy)</p> <p> </p> <p>Further details and code for reading and using these files can be found at the GitHub repo for this paper: <a href="https://github.com/sachalapins/U-GPD">https://github.com/sachalapins/U-GPD</a></p> <p> </p>
Local ground-based geophysical observation data (Borehole tilt, broadband seismic, and infrasound) accompanying the 2018 phreatic eruption at Kusatsu-Shirane volcano (Motoshirane)
<p>A geophysical observation dataset (borehole tilt, broadband seismic, infrasound, and GNSS displacement) accompanying the 2018 phreatic eruption at the Motoshirane cone of the Kusatsu-Shirane volcano. The data was obtained by the local geophysical observation network operated by Kusatsu-Shirane Volcano Observatory, Tokyo Institute of Technology. All time is JST (UTC+9). Terada et al. (2021), Yamada et al. (2021), and Yamada et al. (submitted) describe station locations and instrumentations.</p> <p> </p> <p>Tilt (text files: 20190123_stn_1_Hz.txt)</p> <p>format: yy/mm/dd hour:min sec NS tilt EW tilt</p> <p> </p> <p>Broadband seismic and infrasound waveforms (sac files)</p> <p>(ex: 1801230950_stn_cmp.s)</p> <p>*stn: station name</p> <p>*cmp: component</p> <p> </p> <p>GNSS displacement (pos file)</p> <p>(ex: stn1030_0591.pos)</p> <p>*stn: station name</p> <p>Displacements are calculated by kinematic analysis using 960591 (a GNSS station operated by Geospatial Information Authority of Japan) as a base station. The kinematic analysis was performed on RTKLIB (ver. 2.4.2, Takasu, 2013). See the header for each file for detail.</p> <p> </p> <p> </p> <p>References</p> <p> </p> <p>Terada, A., Kanda, W., Ogawa, Y., Yamada, T., Yamamoto, M., Ohkura, T., et al. (2021). The 2018 phreatic eruption at Mt . Motoshirane of Kusatsu – Shirane volcano, Japan: Eruption and intrusion of hydrothermal fluid observed by a borehole tiltmeter network. Earth, Planets and Space, 73. <a href="https://doi.org/10.1186/s40623-021-01475-4">https://doi.org/10.1186/s40623-021-01475-4</a></p> <p> </p> <p>Takasu, T. (2013), RTKLIB: An Open Source Program Package for GNSS Positioning.</p> <p> </p> <p>Yamada, T., Kurokawa, A. K., Terada, A., Kanda, W., Ueda, H., Aoyama, H., et al. (2021). Locating hydrothermal fluid injection of the 2018 phreatic eruption at Kusatsu-Shirane volcano with volcanic tremor amplitude. Earth, Planets and Space, 73(1), 1–15. https://doi.org/10.1186/s40623-020-01349-1</p>
Bella Coola Seismicity Data
<p>Microseismicity in the western Coast Mountains of British Columbia in the Bella Coola region. Includes initial and relocations of seismicity, P-wave velocity model and station location information, and focal mechanism solutions. These data include detections using the Regressive Estimator (REST) algorithm and those from network analysts at the Geological Survey of Canada (GSC). </p> <p>Files include:</p> <p>1. bella_all_fm.dat</p> <p>All (84) focal mechanism data. Column format is: Lon Lat Depth Strike Dip Rake Magnitude Lon Lat RMS #PolarityMeasurements</p> <p>2. comb_bella_event_3pr.dat<br> All (2,061) 3-pair initial data (Unique GSC, REST, and matched events.)<br> Event header format:</p> <p>YYYY MM DD HH MM SC LAT LON DEP 0 0 0 0 ID</p> <p>3. comb_bella_phase_3pr.dat</p> <p>All (2,061) 3-pair initial data (Unique GSC, REST, and matched events.)<br> Event header format:</p> <p>YYYY MM DD HH MM SC LAT LON DEP 0 0 0 0 ID</p> <p>Phase detection format:<br> Station Traveltime Quality Phase</p> <p>4. event_bella_reloc_mag.dat</p> <p>All (837) final, relocated events from hypoDD.</p> <p>Event header format:</p> <p>YYYY MM DD HH MM SC LAT LON DEP MAG 0 0 0 ID</p> <p>5. phase_bella_reloc.dat</p> <p>All (837) final, relocated events from hypoDD. Includes phase arrival information.</p> <p>Event header format:</p> <p>YYYY MM DD HH MM SC LAT LON DEP MAG 0 0 0 ID</p> <p>Phase detection format:<br> Station Traveltime Quality Phase</p> <p>6. rest_vp.crh</p> <p>1-D P-velocity model used. Column format: P velocity(km/s) Depth(km)</p> <p>7. stationcst.dat</p> <p>Station information. Column format: Name Lat Lon Elevation</p>
Kirchhoff pre-stack depth migration images of the multi-channel seismic data, SO190, RV. SONNE
<p>The dataset consists of four newly processed 2-D pre-stack depth migrated multi-channel seismic lines (BGR06_303, BGR06_305, BGR06_311 and BGR06_313) collected by GEOMAR and BGR in 2006. The dataset reveals the subducted oceanic reliefs and detailed accretionary wedge structure offshore eastern Java, Bali, Lombok, and Sumbawa islands, along the Sunda arc. The dataset is saved in standard SEGY format and could be loaded in open-source or commercial software. </p>
Data files for 'Tan et al., (2022). Seismogenesis of the 2021 Mw 7.1 earthquake sequence near the northeastern Japan revealed by double-difference seismic tomography'
<p>catalog.dat : the selected earthquake phase data (originated from Hi-net, https://www.hinet.bosai.go.jp/?LANG=en)</p> <p>station.dat : the seismic station coordinates</p> <p>MOD : the initial velocity models (including the grid nodes, Vp & Vp/Vs)</p> <p>relocation.dat : the earthquake relocations by the DD tomography</p> <p>Vp_model.dat, Vs_model.dat, VpVs_model.dat : the inverted 3D velocity models by DD tomography (having exactly the same layout as MOD)</p>
Migration of mechanical perturbations estimated by seismic coda wave interferometry during the 2018 pre-eruptive period at Kīlauea volcano, Hawaii : Noise Cross-correlation Functions, Seismic catalog, and GNSS data
<p>ARCHIVE_NCFs_KILAUEA_2018.zip : Compress folder with (1) the daily noise cross-correlation functions (in MSEED format) of the station pairs used in the paper and (2) the one hour noise cross-correlation functions (in H5 format) of the station pairs used in the figure 9 of the paper.</p> <p>Code_Data_HVO.ipynb : Code to download the seismic data, available on IRIS, used in this paper.</p> <p>GPS_data_AHUP.zip : Compress folder with the daily GPS data of the station AHUP used in the paper [Year, Month, Day, Day_of_the_year, Second_of_the_day, East_comp(mm), North_comp(mm), Vertical_comp(mm), Sig_East_comp, Sig_North_comp, Sig_Vertical_comp].</p> <p>Radial_tilt_UWD.txt : Daily radial tilt measurement of the tiltmeter UWD [Year, Month, Day, Radial_tilt(µrad)].</p> <p>Seismic_stations_Kilauea.txt : Name code and location of the seismic stations used in the paper [Station_code, Longitude, Latitude].</p> <p>Seismicity_Catalog_Kilauea_2018_USGS.txt : Seismic catalog from USGS used in the paper [Date_Time, Latitude, Longitude, Depth, Magnitude].</p>
Seismic waveform data near Luding, Sichuan
<p>Regional broadband and short-period waveform datasets are collected to detect and relocate earthquakes during the 2022 M6.8 Luding, Sichuan earthquake sequence. Local broadband and strong-motion waveform datasets are collected to invert focal mechanism solutions of the mainshock and/or some aftershocks.</p> <p><br> Local seismic broadband waveforms with 50 Hz were cut from 5 s before detected P-wave arrivals to 10 s after detected P-wave arrivals. These waveforms were recorded by 54 seismic broadband and short-period stations within 200 km epicenter distances. The dataset for earthquake detection includes used waveforms in miniseed format and result plots in jpeg format.</p> <p><br> Regional seismic broadband event waveforms with 100 Hz were selected for regional Wphase Inversion of the M6.8 mainshock. The epicenter distances of waveforms in SAC format range from 3.0 to 6.0 deg.</p> <p><br> Local seismic broadband waveforms with 100 Hz recorded by stations with ∆ < 350 km were used. The event waveforms in SAC format are available.</p> <p><br> Near-field strong-motion waveforms with 200 Hz by 24 stations are collected to investigate the coseismic rupture history of the mainshock. The strong-motion waveforms start 30 s before the origin time of the mainshock, and last more than 100 s. The event waveform files in dat format are available.</p> <p>Right: Sichuan Earthquake Administration, China Earthquake Administration; Institute of Engineering Mechanics, China Earthquake Administration</p>
Data files for 'Tan et al., (2023). Structural heterogeneity-controlled rupture process of the 2021 Mw 7.1 Fukushima, Japan earthquake revealed by joint inversion of seismic and geodetic data'
<p>slip model.dat: rupture model of the 2021 Mw 7.1 Fukushima earthquake</p> <p>In 'slip model.dat', each row contains the moment rate function of each sub-fault. The numbers of the sub-faults are given in the first two columns.</p>
Seismic node array data for iMUSH shot Y4
<p>Matlab file containing waveform data with a sample rate of 250 Hz from 20 s before to 120 s after shot Y4.</p>
Seismic data Krysuvik Iceland
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Data from: Brittle sedimentary strata focus a multimodal depth distribution of seismicity during hydraulic fracturing in the Sichuan basin, southwest China
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Data from: Seismic low-velocity equatorial torus in the Earth's outer core: Evidence from the late-coda correlation wavefield
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Data from: Subtle shift in groundfish depth distribution within the impact range of seismic surveying along a continental slope
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Data from: Knowledge graphs for seismic data and metadata
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Seismic and Pressure data for Wang and Tanimoto
<p>Seismic and pressure data output files used for calculating half-space rigidity values at TA stations. </p>
Data and figures of JGR planet paper entitled "Pressure effects on the SEIS-InSight instrument, improvement of seismic records and characterization of long period atmospheric waves from ground displacements" by Raphael F. Garcia and co-authors
<p>Data and figures of the JGR Planet paper entitled "Pressure effects on the SEIS-<br> InSight instrument, improvement of seismic records and characterization of long<br> period atmospheric waves from ground displacements"<br> by<br> Raphael F. Garcia1, Balthasar Kenda2 , Taichi Kawamura2 , A. Spiga3,4, N.<br> Murdoch1 , P. Lognonné2, R. Widmer-Schnidrig5, N. Compaire1 , G.<br> Orhand-Mainsant1 , D. Banfield6, W. B. Banerdt7</p> <p>List of files and directories</p> <p>*extractAllDataFromFig.m : matlab code to extract the data in txt file from the<br> matlab figures listed in the following directories<br> Figure1<br> Figure10<br> Figure11<br> Figure2<br> Figure3<br> Figure4<br> Figure5<br> Figure6<br> Figure7<br> Figure8<br> Figure9</p> <p>*figures_combined : combined figures for JGR paper</p> <p>*INSIGHT_Data : data in miniseed format used in the paper<br> -- Deglitch_data : data after removing glitchs used in the paper<br> -- Data_figure11 : data used for the plots in figure 11 (plots done easily with<br> SeisGram software)</p> <p>*PREPRINT : preprint of the paper</p> <p> </p>
Data from: Friction of Longmaxi shale gouges and implications for seismicity during hydraulic fracturing
<p>Longmaxi formation shales are the major target reservoir for shale gas extraction in the Sichuan Basin, southwest China. Swarms of earthquakes accompanying hydraulic fracturing are observed at depths typified by the Longmaxi formation. Mineral composition varies broadly through the stratigraphic section due to different depositional environments. The section is generally tectosilicate-poor and phyllosilicate-rich with a minor portion (~5 <i>wt</i>.%) the converse. We measure the frictional and stability properties of shale gouges taken from the full stratigraphic section at hydrothermal conditions. Velocity-stepping experiments were performed on representative shale gouges at <i>σ<sub>c</sub></i> = 60 <i>MPa</i>, <i>P<sub>f</sub></i> = 30 <i>MPa</i> and <i>T</i> =150 <i>℃</i>. Results show that the gouges are generally frictionally strong with friction coefficients spanning a range of 0.50-0.75. Two phyllosilicate+TOC-poor gouges exhibited higher frictional strength and velocity weakening behavior, capable of potentially unstable fault slips, while only velocity strengthening behavior was observed for the remaining phyllosilicate+TOC-rich gouges. These results confirm that the frictional and stability properties are mainly controlled by phyllosilicate+TOC content. Elevating the temperature further weakens the gouges and drives it towards velocity weakening. The presence of observed seismicity in majority velocity strengthening materials suggest the importance of the minority velocity weakening materials. We suggest a model where seismicity is triggered when high pore fluid pressures drive aseismic slip in the near-field and triggers seismic slip on adjacent faults. Our results have important implications in understanding the physics of earthquakes in Sichuan Basin and highlights the importance of identifying the location and characteristics of faults prior to hydraulic fracturing.</p>
Towards automated early detection of risks for a CO2 plume containment from permanent seismic monitoring data
<p>This storage contains the training data for neural networks proposed in a manuscript 'Towards automated early detection of risks for a CO2 plume containment from permanent seismic monitoring data'. The data consists of output from reservoir simulations of a small-scale CO2 injection at CO2CRC Otway Project Stage 2C (Victoria, Australia). The output is presented as a set of images, where each pixel in a portable network graphics is a plume thickness for a particular injection scenario at a particular day after the injection has commenced. The format is unsigned integer 16-bit. The data set contains images of two major types:</p> <p>1. REALISTIC: plumes are obtained from reservoir simulations in a complex geological model that was calibrated on an extensive set of geophysical surveys. File naming follows this convention 'plume_thick_real_scenario_%S_day_%N.png', where %S represents a string that encodes the injection scenario name and %N denotes day number after the injection started.</p> <p>2. VANILLA: plumes are obtained from reservoir simulations in a simple model of a reservoir that reflects only few typical features of the Otway injection interval. 'plume_thick_vanilla_scenario_%S_day_%N.png', where %S represents a string that encodes the injection scenario name and %N denotes day number after the injection started.</p>
Data: Effects of seismic airgun playbacks on swimming patterns and behavioural states of Atlantic cod in a net pen
<p>Data abstract:</p> <p>We tracked individual fish using acoustic telemetry and exposed them to sound. Here, we provide (1) the raw acoustic tag detections, (2) the filtered/processed tag detections which served as an input for YAPS (Yet Another Positioning Solver), (3) the positions of the hydrophones (acoustic tag receivers), and (4) the positions of the fish (output of YAPS) and other relevant covariates (sun elevation, tide and treatment period).</p> <p> </p> <p>Paper abstract:</p> <p>Anthropogenic sound can affect fish behaviour and physiology which may affect their well-being. However, it remains a major challenge to translate such effects to consequences for fitness at an individual and population level. For this, energy budget models have been developed, but suitable data to parametrize these models are lacking. A first step towards such parametrization concerns the objective quantification of behavioural states at high resolution. We experimentally exposed individual Atlantic cod (<em>Gadus morhua</em>) in a net pen to the playback of seismic airgun sounds. We demonstrated that individual cod in the net pen did not change their swimming patterns immediately at the onset of the sound exposure. However, several individuals changed their time expenditure in three different behavioural states during the 1 h exposure. This may be suitable input for energy budget models that allow predictions about fitness consequences of acoustic disturbance.</p> <p> </p> <p>Paper reference:</p> <p>Hubert, J., Campbell, J. A., Slabbekoorn, H. (2020). Effects of seismic airgun playbacks on swimming patterns and behavioural states of Atlantic cod in a net pen. <em>Mar. Pollut. Bull.</em> <strong>160</strong>, 111680. DOI:10.1016/j.marpolbul.2020.111680</p>
Data supporting tables and figures in t ms Tidal influence on seismic activity during the 2011-2013 El Hierro volcanic unrest
<p>Introduction</p> <p>This set of files contains data supporting the tables and figures featured in the journal article.<br> <br> File Ts01.xlsx shows data from the earthquake cluster C1 defined in the manuscript, as well as tidal stress phases and amplitudes obtained for each event using the methodology explained in the text. <br> Files Ts02.xlsx, Ts03.xlsx and Ts04.xlsx are datasets analog to File Ts01.xlsx, but using data from clusters C2, C3 and C4 respectively. <br> Data of Files Ts01.xlsx, Ts02.xlsx, Ts03.xlsx and Ts04.xlsx have been used to compose Tables 1, 2, 3, 4, 5, 6 in the manuscript, Figures 3, 5, 8, 9 in the manuscript, <br> plus Figures S9, S10, S11, S12, S13, S14, S15, S16 in the Supporting Information.</p> <p>File Ts05.xlsx features tidal strain calculated for the setting of the shallow magma reservior in Phase 1 of the volcanic crisis, at two-hour intervals, between 2011-07-01 and 2011-10-31. <br> Data from File Ts05.xlsx has been used for composition of Figures 6 and 7 in the manuscript.<br> Files Ts06.xlsx, Ts07.xlsx and Ts08.xlsx are datasets analog to File Ts05.xlsx, but calculating tidal strain for the locations of events belonging to clusters C2, C3 and C4 respectively.<br> Data of Files Ts06.xlsx, Ts07.xlsx and Ts08.xlsx have been used to compose Figures S1, S2, S3, S4, S5, S6 in the Supporting Information. </p> <p>File Ts09.xlsx shows tidal confining stress values corresponding to the events in cluster C1. <br> File Ts10.xlsx features values of tidal stress taken hourly for the location corresponding to an event belonging to subcluster C1A. <br> File Ts11.xlsx features values of tidal stress taken hourly for the location corresponding to an event belonging to subcluster C1B. <br> Figure S7 in the Supporting Information has been produced using data from Files Ts09.xlsx, Ts10.xlsx and Ts11.xlsx. </p> <p>File Ts12.xlsx collects all events in four clusters C1-C4, and shows the amplitudes of the tidal confining stress half cycles in which the events occur, considering only ocean tides or only body tides. <br> These data were used for stating the predominance of ocean tidal loading against body tides in Chapter 5 - Discussion.</p> <p>File Ts13.xlsx shows data from the earthquake cluster C1 defined in the manuscript, as well as tidal stress phases and amplitudes, but considering only those events with M >= 2.<br> Files Ts14.xlsx, Ts15.xlsx and Ts16.xlsx are datasets analog to File Ts13.xlsx, but using data from clusters C2, C3 and C4 (events with M >= 2 only) respectively.<br> Data of Files Ts13.xlsx, Ts14.xlsx, Ts15.xlsx and Ts16.xlsx have been used to compose Table S3 in the Supporting Information.</p> <p>File Ts17.xlsx features the 4 declustered catalogs D1, D2, D3 and D4 which are described in Tables S4 and S5 in the Supporting Information.</p> <p>File Ts18.xlsx collects all events in four clusters C1-C4, and shows the results of tidal tilt (North-South and East-West components). <br> These data were used to compose Figures S27 and S28 in the Supporting Information. </p> <p>File Ts19.xlsx features tidal stress calculated for the setting of the shallow magma reservior in Phase 1 of the volcanic crisis, at two-hour intervals, between 2011-07-01 and 2011-10-31. <br> Data from File Ts19.xlsx has been used for composition of Figure S17 in the manuscript.<br> Files Ts20.xlsx, Ts21.xlsx and Ts22.xlsx are datasets analog to File Ts19.xlsx, but calculating tidal stress for the locations of events belonging to clusters C2, C3 and C4 respectively.<br> Data of Files Ts20.xlsx, Ts21.xlsx and Ts22.xlsx have been used to compose Figures S18, S19 and S20 in the Supporting Information.</p> <p>File Ts23.xlsx shows data from the earthquake cluster C1 defined in the manuscript, as well as tidal stress phases and amplitudes obtained for each event using the methodology explained in the text,<br> but considering only ocean tides in the calculations. <br> Files Ts24.xlsx, Ts25.xlsx and Ts26.xlsx are datasets analog to File Ts23.xlsx, but using data from clusters C2, C3 and C4 respectively. <br> Data of Files Ts01.xlsx, Ts02.xlsx, Ts03.xlsx and Ts04.xlsx have been used to compose Figures S21 and S22 in Supporting Information.</p> <p>File Ts27.xlsx features horizontal tidal stress (Earth tides only) calculated for the setting of the shallow magma reservior in Phase 1 of the volcanic crisis, at two-hour intervals, <br> between 2011-07-01 and 2011-10-31. Data from File Ts27.xlsx has been used for composition of Figure S23 in the manuscript.<br> Files Ts28.xlsx, Ts29.xlsx and Ts30.xlsx are datasets analog to File Ts27.xlsx, but calculating horizontal tidal stress for the locations of events belonging to clusters C2, C3 and C4 respectively.<br> Data of Files Ts28.xlsx, Ts29.xlsx and Ts30.xlsx have been used to compose Figures S24, S25 and S26 in the Supporting Information.</p> <p>1. Ts01.xlsx Data used to detect tidal stress correlations in Phase 1 of the volcanic crisis.</p> <p>1.1 Column "Year", y.<br> 1.2 Column "Month", m.<br> 1.3 Column "Day", d.<br> 1.4 Column "Hour", h.<br> 1.5 Column "Minute", min.<br> 1.6 Column "Second", s.<br> 1.7 Column "Latitude", deg, latitude north of equator.<br> 1.8 Column "Longitude", deg, longitude east of Greenwich.<br> 1.9 Column "Depth", km.<br> 1.10 Column "Phase_east-west_stress", deg, tidal phase angle assigned to the event, calculated for tidal east-west stress.<br> 1.11 Column "Amplitude_east-west_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal east-west stress.<br> 1.12 Column "Phase_north-south_stress", deg, tidal phase angle assigned to the event, calculated for tidal north-south stress.<br> 1.13 Column "Amplitude_north-south_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal north-south stress.<br> 1.14 Column "Phase_vertical_stress", deg, tidal phase angle assigned to the event, calculated for tidal vertical stress.<br> 1.15 Column "Amplitude_vertical_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal vertical stress.<br> 1.16 Column "Phase_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 1.17 Column "Amplitude_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 1.18 Column "Phase_confining_stress_rate", deg, tidal phase angle assigned to the event, calculated for tidal confining stress rate.<br> 1.19 Column "Amplitude_confining_stress_rate", Pa/h, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress rate.<br> 1.20 Column "Magnitude", earthquake magnitude.<br> 1.21 Column "Autonum", autonumeric code.</p> <p>2. Ts02.xlsx Data used to detect tidal stress correlations in Phase 2 of the volcanic crisis.</p> <p>2.1 Column "Year", y.<br> 2.2 Column "Month", m.<br> 2.3 Column "Day", d.<br> 2.4 Column "Hour", h.<br> 2.5 Column "Minute", min.<br> 2.6 Column "Second", s.<br> 2.7 Column "Latitude", deg, latitude north of equator.<br> 2.8 Column "Longitude", deg, longitude east of Greenwich.<br> 2.9 Column "Depth", km.<br> 2.10 Column "Phase_east-west_stress", deg, tidal phase angle assigned to the event, calculated for tidal east-west stress.<br> 2.11 Column "Amplitude_east-west_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal east-west stress.<br> 2.12 Column "Phase_north-south_stress", deg, tidal phase angle assigned to the event, calculated for tidal north-south stress.<br> 2.13 Column "Amplitude_north-south_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal north-south stress.<br> 2.14 Column "Phase_vertical_stress", deg, tidal phase angle assigned to the event, calculated for tidal vertical stress.<br> 2.15 Column "Amplitude_vertical_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal vertical stress.<br> 2.16 Column "Phase_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 2.17 Column "Amplitude_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 2.18 Column "Phase_confining_stress_rate", deg, tidal phase angle assigned to the event, calculated for tidal confining stress rate.<br> 2.19 Column "Amplitude_confining_stress_rate", Pa/h, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress rate.<br> 2.20 Column "Magnitude", earthquake magnitude.<br> 2.21 Column "Autonum", autonumeric code.</p> <p>3. Ts03.xlsx Data used to detect tidal stress correlations in Phase 3 of the volcanic crisis.</p> <p>3.1 Column "Year", y.<br> 3.2 Column "Month", m.<br> 3.3 Column "Day", d.<br> 3.4 Column "Hour", h.<br> 3.5 Column "Minute", min.<br> 3.6 Column "Second", s.<br> 3.7 Column "Latitude", deg, latitude north of equator.<br> 3.8 Column "Longitude", deg, longitude east of Greenwich.<br> 3.9 Column "Depth", km.<br> 3.10 Column "Phase_east-west_stress", deg, tidal phase angle assigned to the event, calculated for tidal east-west stress.<br> 3.11 Column "Amplitude_east-west_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal east-west stress.<br> 3.12 Column "Phase_north-south_stress", deg, tidal phase angle assigned to the event, calculated for tidal north-south stress.<br> 3.13 Column "Amplitude_north-south_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal north-south stress.<br> 3.14 Column "Phase_vertical_stress", deg, tidal phase angle assigned to the event, calculated for tidal vertical stress.<br> 3.15 Column "Amplitude_vertical_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal vertical stress.<br> 3.16 Column "Phase_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 3.17 Column "Amplitude_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 3.18 Column "Phase_confining_stress_rate", deg, tidal phase angle assigned to the event, calculated for tidal confining stress rate.<br> 3.19 Column "Amplitude_confining_stress_rate", Pa/h, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress rate.<br> 3.20 Column "Magnitude", earthquake magnitude.<br> 3.21 Column "Autonum", autonumeric code.</p> <p>4. Ts04.xlsx Data used to detect tidal stress correlations in Phase 4 of the volcanic crisis.</p> <p>4.1 Column "Year", y.<br> 4.2 Column "Month", m.<br> 4.3 Column "Day", d.<br> 4.4 Column "Hour", h.<br> 4.5 Column "Minute", min.<br> 4.6 Column "Second", s.<br> 4.7 Column "Latitude", deg, latitude north of equator.<br> 4.8 Column "Longitude", deg, longitude east of Greenwich.<br> 4.9 Column "Depth", km.<br> 4.10 Column "Phase_east-west_stress", deg, tidal phase angle assigned to the event, calculated for tidal east-west stress.<br> 4.11 Column "Amplitude_east-west_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal east-west stress.<br> 4.12 Column "Phase_north-south_stress", deg, tidal phase angle assigned to the event, calculated for tidal north-south stress.<br> 4.13 Column "Amplitude_north-south_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal north-south stress.<br> 4.14 Column "Phase_vertical_stress", deg, tidal phase angle assigned to the event, calculated for tidal vertical stress.<br> 4.15 Column "Amplitude_vertical_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal vertical stress.<br> 4.16 Column "Phase_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 4.17 Column "Amplitude_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 4.18 Column "Phase_confining_stress_rate", deg, tidal phase angle assigned to the event, calculated for tidal confining stress rate.<br> 4.19 Column "Amplitude_confining_stress_rate", Pa/h, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress rate.<br> 4.20 Column "Magnitude", earthquake magnitude.<br> 4.21 Column "Autonum", autonumeric code.</p> <p>5. Ts05.xlsx Tidal strain calculated for the shallow magma reservior between 2011-07-01 and 2011-10-31.</p> <p>5.1 Column "Latitude", deg, latitude north of equator.<br> 5.2 Column "Longitude", deg, longitude east of Greenwich.<br> 5.3 Column "Depth", km.<br> 5.4 Column "Date", date in format yyyymmdd.<br> 5.5 Column "Time", time in format hour : minute : second.<br> 5.6 Column "Volume strain", nanostrain, tidal volume strain.<br> 5.7 Column "East-West strain", nanostrain, tidal East-West strain.<br> 5.8 Column "North-South strain", nanostrain, tidal North-South strain.<br> 5.9 Column "Vertical strain", nanostrain, tidal Vertical strain.</p> <p>6. Ts06. Tidal strain calculated for the location of an event belonging to cluster C2.</p> <p>6.1 Column "Latitude", deg, latitude north of equator.<br> 6.2 Column "Longitude", deg, longitude east of Greenwich.<br> 6.3 Column "Depth", km.<br> 6.4 Column "Date", date in format yyyymmdd.<br> 6.5 Column "Time", time in format hour : minute : second.<br> 6.6 Column "Volume strain", nanostrain, tidal volume strain.<br> 6.7 Column "East-West strain", nanostrain, tidal East-West strain.<br> 6.8 Column "North-South strain", nanostrain, tidal North-South strain.<br> 6.9 Column "Vertical strain", nanostrain, tidal Vertical strain.</p> <p>7. Ts07. Tidal strain calculated for the location of an event belonging to cluster C3.</p> <p>7.1 Column "Latitude", deg, latitude north of equator.<br> 7.2 Column "Longitude", deg, longitude east of Greenwich.<br> 7.3 Column "Depth", km.<br> 7.4 Column "Date", date in format yyyymmdd.<br> 7.5 Column "Time", time in format hour : minute : second.<br> 7.6 Column "Volume strain", nanostrain, tidal volume strain.<br> 7.7 Column "East-West strain", nanostrain, tidal East-West strain.<br> 7.8 Column "North-South strain", nanostrain, tidal North-South strain.<br> 7.9 Column "Vertical strain", nanostrain, tidal Vertical strain.</p> <p>8. Ts08. Tidal strain calculated for the location of an event belonging to cluster C4.</p> <p>8.1 Column "Latitude", deg, latitude north of equator.<br> 8.2 Column "Longitude", deg, longitude east of Greenwich.<br> 8.3 Column "Depth", km.<br> 8.4 Column "Date", date in format yyyymmdd.<br> 8.5 Column "Time", time in format hour : minute : second.<br> 8.6 Column "Volume strain", nanostrain, tidal volume strain.<br> 8.7 Column "East-West strain", nanostrain, tidal East-West strain.<br> 8.8 Column "North-South strain", nanostrain, tidal North-South strain.<br> 8.9 Column "Vertical strain", nanostrain, tidal Vertical strain.</p> <p>9. File Ts09.xlsx Tidal confining stress values corresponding to the events in cluster C1.</p> <p>9.1 Column "Latitude", deg, latitude north of equator.<br> 9.2 Column "Longitude", deg, longitude east of Greenwich.<br> 9.3 Column "Depth", km.<br> 9.4 Column "Date", date in format yyyymmdd.<br> 9.5 Column "Time", time in format hour : minute : second.<br> 9.6 Column "Tides", Pa, tidal confining stress.</p> <p>10. Ts10.xlsx Hourly values of tidal confining stress obtained for the location of an earthquake belonging to subcluster C1A.</p> <p>10.1 Column "Year", y.<br> 10.2 Column "Month", m.<br> 10.3 Column "Day", d.<br> 10.4 Column "Hour", h.<br> 10.5 Column "Minute", min.<br> 10.6 Column "Second", s.<br> 10.7 Column "Latitude", deg, latitude north of equator.<br> 10.8 Column "Longitude", deg, longitude east of Greenwich.<br> 10.9 Column "Depth", m.<br> 10.10 Column "Tides", Pa, tidal confining stress.</p> <p>11. Ts11.xlsx Hourly values of tidal confining stress obtained for the location of an earthquake belonging to subcluster C1B.</p> <p>11.1 Column "Year", y.<br> 11.2 Column "Month", m.<br> 11.3 Column "Day", d.<br> 11.4 Column "Hour", h.<br> 11.5 Column "Minute", min.<br> 11.6 Column "Second", s.<br> 11.7 Column "Latitude", deg, latitude north of equator.<br> 11.8 Column "Longitude", deg, longitude east of Greenwich.<br> 11.9 Column "Depth", m.<br> 11.10 Column "Tides", Pa, tidal confining stress.</p> <p>12. Ts12.xlsx Data used to compare ocean tides to body tides</p> <p>12.1 Column "Cluster", number of the cluster (C1-C4).<br> 12.2 Column "Year", y.<br> 12.3 Column "Month", m.<br> 12.4 Column "Day", d.<br> 12.5 Column "Hour", h.<br> 12.6 Column "Minute", min.<br> 12.7 Column "Second", s.<br> 12.8 Column "Latitude", deg, latitude north of equator.<br> 12.9 Column "Longitude", deg, longitude east of Greenwich.<br> 12.10 Column "Depth", km.<br> 12.11 Column "Autonum", autonumeric code.<br> 12.12 Column "Ampl_ocean_hc", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress, ocean tides only.<br> 12.13 Column "Ampl_body_hc", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress, body tides only.</p> <p>13. Ts13.xlsx Data in Cluster C1 with M>=2</p> <p>13.1 Column "Year", y.<br> 13.2 Column "Month", m.<br> 13.3 Column "Day", d.<br> 13.4 Column "Hour", h.<br> 13.5 Column "Minute", min.<br> 13.6 Column "Second", s.<br> 13.7 Column "Latitude", deg, latitude north of equator.<br> 13.8 Column "Longitude", deg, longitude east of Greenwich.<br> 13.9 Column "Depth", km.<br> 13.10 Column "Phase_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 13.11 Column "Amplitude_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 13.12 Column "Magnitude", earthquake magnitude.<br> 13.13 Column "Autonum", autonumeric code.</p> <p>14. Ts14.xlsx Data in Cluster C2 with M>=2</p> <p>14.1 Column "Year", y.<br> 14.2 Column "Month", m.<br> 14.3 Column "Day", d.<br> 14.4 Column "Hour", h.<br> 14.5 Column "Minute", min.<br> 14.6 Column "Second", s.<br> 14.7 Column "Latitude", deg, latitude north of equator.<br> 14.8 Column "Longitude", deg, longitude east of Greenwich.<br> 14.9 Column "Depth", km.<br> 14.10 Column "Phase_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 14.11 Column "Amplitude_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 14.12 Column "Magnitude", earthquake magnitude.<br> 14.13 Column "Autonum", autonumeric code.</p> <p>15. Ts15.xlsx Data in Cluster C3 with M>=2</p> <p>15.1 Column "Year", y.<br> 15.2 Column "Month", m.<br> 15.3 Column "Day", d.<br> 15.4 Column "Hour", h.<br> 15.5 Column "Minute", min.<br> 15.6 Column "Second", s.<br> 15.7 Column "Latitude", deg, latitude north of equator.<br> 15.8 Column "Longitude", deg, longitude east of Greenwich.<br> 15.9 Column "Depth", km.<br> 15.10 Column "Phase_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 15.11 Column "Amplitude_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 15.12 Column "Magnitude", earthquake magnitude.<br> 15.13 Column "Autonum", autonumeric code.</p> <p>16. Ts16.xlsx Data in Cluster C4 with M>=2</p> <p>16.1 Column "Year", y.<br> 16.2 Column "Month", m.<br> 16.3 Column "Day", d.<br> 16.4 Column "Hour", h.<br> 16.5 Column "Minute", min.<br> 16.6 Column "Second", s.<br> 16.7 Column "Latitude", deg, latitude north of equator.<br> 16.8 Column "Longitude", deg, longitude east of Greenwich.<br> 16.9 Column "Depth", km.<br> 16.10 Column "Phase_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 16.11 Column "Amplitude_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 16.12 Column "Magnitude", earthquake magnitude.<br> 16.13 Column "Autonum", autonumeric code.</p> <p>17. Ts17.xlsx Declustered datasets D1, D2, D3 and D4</p> <p>17.1 Column "Dataset", number of the declustered dataset (D1-D4).<br> 17.2 Column "Year", y.<br> 17.3 Column "Month", m.<br> 17.4 Column "Day", d.<br> 17.5 Column "Latitude", deg, latitude north of equator.<br> 17.6 Column "Longitude", deg, longitude east of Greenwich.<br> 17.7 Column "Magnitude", earthquake magnitude.<br> 17.8 Column "Depth", km.<br> 17.9 Column "Cluster". It takes the value "+" if the event does not belong to any cluster identified during the declustering process. <br> Otherwise, the event is the largest in a cluster identified by the code shown in Table S4 in Supporting Information. </p> <p><br> 18. Ts18.xlsx Data used to detect tidal tilt correlations</p> <p>18.1 Column "Cluster", number of the cluster (C1-C4).<br> 18.2 Column "Year", y.<br> 18.3 Column "Month", m.<br> 18.4 Column "Day", d.<br> 18.5 Column "Hour", h.<br> 18.6 Column "Minute", min.<br> 18.7 Column "Second", s.<br> 18.8 Column "Latitude", deg, latitude north of equator.<br> 18.9 Column "Longitude", deg, longitude east of Greenwich.<br> 18.10 Column "Depth", km.<br> 18.11 Column "Autonum", autonumeric code.<br> 18.12 Column "Phase_tilt_NS", deg, tidal phase angle assigned to the event, calculated for tidal tilt (North-South component).<br> 18.13 Column "Ampl_tilt_NS", nrad, amplitude of the tidal half cycle in which the event occurs, calculated for tidal tilt (North-South component).<br> 18.14 Column "Phase_tilt_EW", deg, tidal phase angle assigned to the event, calculated for tidal tilt (East-West component).<br> 18.15 Column "Ampl_tilt_NS", nrad, amplitude of the tidal half cycle in which the event occurs, calculated for tidal tilt (East-West component).</p> <p>19. Ts19.xlsx Tidal stress calculated for the shallow magma reservior between 2011-07-01 and 2011-10-31.</p> <p>19.1 Column "Latitude", deg, latitude north of equator.<br> 19.2 Column "Longitude", deg, longitude east of Greenwich.<br> 19.3 Column "Depth", km.<br> 19.4 Column "Date", date in format yyyymmdd.<br> 19.5 Column "Time", time in format hour : minute : second.<br> 19.6 Column "East-West stress", Pa, tidal East-West stress.<br> 19.7 Column "North-South stress", Pa, tidal North-South stress.<br> 19.8 Column "Vertical stress", Pa, tidal Vertical stress.</p> <p>20. Ts20.xlsx Tidal stress calculated for the location of an event belonging to cluster C2.</p> <p>20.1 Column "Latitude", deg, latitude north of equator.<br> 20.2 Column "Longitude", deg, longitude east of Greenwich.<br> 20.3 Column "Depth", km.<br> 20.4 Column "Date", date in format yyyymmdd.<br> 20.5 Column "Time", time in format hour : minute : second.<br> 20.6 Column "East-West stress", Pa, tidal East-West stress.<br> 20.7 Column "North-South stress", Pa, tidal North-South stress.<br> 20.8 Column "Vertical stress", Pa, tidal Vertical stress.</p> <p>21. Ts21.xlsx Tidal stress calculated for the location of an event belonging to cluster C3.</p> <p>21.1 Column "Latitude", deg, latitude north of equator.<br> 21.2 Column "Longitude", deg, longitude east of Greenwich.<br> 21.3 Column "Depth", km.<br> 21.4 Column "Date", date in format yyyymmdd.<br> 21.5 Column "Time", time in format hour : minute : second.<br> 21.6 Column "East-West stress", Pa, tidal East-West stress.<br> 21.7 Column "North-South stress", Pa, tidal North-South stress.<br> 21.8 Column "Vertical stress", Pa, tidal Vertical stress.</p> <p>22. Ts22.xlsx Tidal stress calculated for the location of an event belonging to cluster C4.</p> <p>22.1 Column "Latitude", deg, latitude north of equator.<br> 22.2 Column "Longitude", deg, longitude east of Greenwich.<br> 22.3 Column "Depth", km.<br> 22.4 Column "Date", date in format yyyymmdd.<br> 22.5 Column "Time", time in format hour : minute : second.<br> 22.6 Column "East-West stress", Pa, tidal East-West stress.<br> 22.7 Column "North-South stress", Pa, tidal North-South stress.<br> 22.8 Column "Vertical stress", Pa, tidal Vertical stress.</p> <p>23. Ts23.xlsx Data used to detect tidal stress correlations in Phase 1 of the volcanic crisis (ocean tides only).</p> <p>23.1 Column "Year", y.<br> 23.2 Column "Month", m.<br> 23.3 Column "Day", d.<br> 23.4 Column "Hour", h.<br> 23.5 Column "Minute", min.<br> 23.6 Column "Second", s.<br> 23.7 Column "Latitude", deg, latitude north of equator.<br> 23.8 Column "Longitude", deg, longitude east of Greenwich.<br> 23.9 Column "Depth", km.<br> 23.10 Column "Phase_ocean_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 23.11 Column "Amplitude_ocean_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 23.12 Column "Magnitude", earthquake magnitude.<br> 23.13 Column "Autonum", autonumeric code.</p> <p>24. Ts24.xlsx Data used to detect tidal stress correlations in Phase 2 of the volcanic crisis (ocean tides only).</p> <p>24.1 Column "Year", y.<br> 24.2 Column "Month", m.<br> 24.3 Column "Day", d.<br> 24.4 Column "Hour", h.<br> 24.5 Column "Minute", min.<br> 24.6 Column "Second", s.<br> 24.7 Column "Latitude", deg, latitude north of equator.<br> 24.8 Column "Longitude", deg, longitude east of Greenwich.<br> 24.9 Column "Depth", km.<br> 24.10 Column "Phase_ocean_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 24.11 Column "Amplitude_ocean_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 24.12 Column "Magnitude", earthquake magnitude.<br> 24.13 Column "Autonum", autonumeric code.</p> <p>25. Ts25.xlsx Data used to detect tidal stress correlations in Phase 3 of the volcanic crisis (ocean tides only).</p> <p>25.1 Column "Year", y.<br> 25.2 Column "Month", m.<br> 25.3 Column "Day", d.<br> 25.4 Column "Hour", h.<br> 25.5 Column "Minute", min.<br> 25.6 Column "Second", s.<br> 25.7 Column "Latitude", deg, latitude north of equator.<br> 25.8 Column "Longitude", deg, longitude east of Greenwich.<br> 25.9 Column "Depth", km.<br> 25.10 Column "Phase_ocean_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 25.11 Column "Amplitude_ocean_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 25.12 Column "Magnitude", earthquake magnitude.<br> 25.13 Column "Autonum", autonumeric code.</p> <p>26. Ts26.xlsx Data used to detect tidal stress correlations in Phase 4 of the volcanic crisis (ocean tides only).</p> <p>26.1 Column "Year", y.<br> 26.2 Column "Month", m.<br> 26.3 Column "Day", d.<br> 26.4 Column "Hour", h.<br> 26.5 Column "Minute", min.<br> 26.6 Column "Second", s.<br> 26.7 Column "Latitude", deg, latitude north of equator.<br> 26.8 Column "Longitude", deg, longitude east of Greenwich.<br> 26.9 Column "Depth", km.<br> 26.10 Column "Phase_ocean_confining_stress", deg, tidal phase angle assigned to the event, calculated for tidal confining stress.<br> 26.11 Column "Amplitude_ocean_confining_stress", Pa, amplitude of the tidal half cycle in which the event occurs, calculated for tidal confining stress.<br> 26.12 Column "Magnitude", earthquake magnitude.<br> 26.13 Column "Autonum", autonumeric code.</p> <p>27. Ts27.xlsx Horizontal tidal stress (Earth tides only) calculated for the shallow magma reservior between 2011-07-01 and 2011-10-31.</p> <p>27.1 Column "Latitude", deg, latitude north of equator.<br> 27.2 Column "Longitude", deg, longitude east of Greenwich.<br> 27.3 Column "Depth", km.<br> 27.4 Column "Date", date in format yyyymmdd.<br> 27.5 Column "Time", time in format hour : minute : second.<br> 27.6 Column "Horizontal stress", Pa, tidal Horizontal stress.</p> <p>28. Ts28.xlsx Horizontal tidal stress (Earth tides only) calculated for the location of an event belonging to cluster C2.</p> <p>28.1 Column "Latitude", deg, latitude north of equator.<br> 28.2 Column "Longitude", deg, longitude east of Greenwich.<br> 28.3 Column "Depth", km.<br> 28.4 Column "Date", date in format yyyymmdd.<br> 28.5 Column "Time", time in format hour : minute : second.<br> 28.6 Column "Horizontal stress", Pa, tidal Horizontal stress.</p> <p>29. Ts29.xlsx Horizontal tidal stress (Earth tides only) calculated for the location of an event belonging to cluster C3.</p> <p>29.1 Column "Latitude", deg, latitude north of equator.<br> 29.2 Column "Longitude", deg, longitude east of Greenwich.<br> 29.3 Column "Depth", km.<br> 29.4 Column "Date", date in format yyyymmdd.<br> 29.5 Column "Time", time in format hour : minute : second.<br> 29.6 Column "Horizontal stress", Pa, tidal Horizontal stress.</p> <p>30. Ts30.xlsx Horizontal tidal stress (Earth tides only) calculated for the location of an event belonging to cluster C4.</p> <p>30.1 Column "Latitude", deg, latitude north of equator.<br> 30.2 Column "Longitude", deg, longitude east of Greenwich.<br> 30.3 Column "Depth", km.<br> 30.4 Column "Date", date in format yyyymmdd.<br> 30.5 Column "Time", time in format hour : minute : second.<br> 30.6 Column "Horizontal stress", Pa, tidal Horizontal stress.</p>
ScienceDex guides
Understand access before you commit
These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
Allen Brain Atlas
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DANDI Archive for NWB datasets
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International Brain Laboratory public data
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OpenNeuro
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