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662 results for “seismicity”

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zenodo32/100

Supplementary Dataset for the Report "Imaging the Western Edge of the Aegean Shear Zone: The South Evia 2022-2023 Seismic Sequence"

<p>Supplementary Dataset for the Fast Report &quot;<strong>Imaging the Western Edge of the Aegean Shear Zone: The South Evia 2022-2023 Seismic Sequence</strong>&quot; by Christos P. Evangelidis and Ioannis Fountoulakis.</p> <p>The Fast Report can be found in <em><strong>Seismica Vol. 2 No. 1 (2023)</strong></em>.</p> <p><strong>DOI:</strong> <a href="https://doi.org/10.26443/seismica.v2i1.1032">https://doi.org/10.26443/seismica.v2i1.1032</a></p> <p><em><strong>Abstract:</strong></em></p> <p>This report presents the 2022-2023 South Evia island seismic sequence, in the western Aegean sea. An automated workflow, undergoing testing for efficient observatory monitoring in the wake of dense aftershock sequences, was employed to enhance the seismic catalog. It includes a deep-learning phase picker, absolute and relative hypocenter relocation, and moment tensor automatic calculations. The relocated catalog reveals a concentration of earthquake epicenters in a narrow NW-SE zone, with sinistral strike-slip fault movement. The findings of the study indicate the occurrence of an asymmetric rupture within conjugate fault structures in the western Aegean region. These fault structures, although not necessarily both active, play a significant role in marking the transition from dextral (SW-NE) to sinistral (NW-SE) strike-slip ruptures, connecting the Aegean shear zone with normal faulting in mainland Greece. The South Evia 2022-2023 seismic sequence has revealed the activation of this NW-SE strike-slip structure, contrary to previous assumptions of low seismicity in the region. The study highlights the importance of reassessing seismic hazard maps and considering the potential activation of similar zones further south in the future. It also emphasizes the need for the expansion and the densification of seismic networks within the Aegean.</p> <p><em><strong>Files:</strong></em></p> <p><strong>Relocated_Catalog.txt</strong>: Relocated earthquake catalog for the South Evia sequence. Included in the document are details concerning the origin time, the hypocentral positions, errors in determining the location, and the local magnitude of each earthquake.</p>

opencc-by-4.0Jun 2023View details →
zenodo32/100

Data files for 'Tan et al., (2020). Hydraulic fracturing induced seismicity in the southern Sichuan Basin due to fluid diffusion inferred from seismic and injection data analysis'

<p>CEDC catalog.xlsx : the seismic catalog from China Earthquake Data Center (https://data.earthquake.cn/)</p> <p>Local network catalog.xlsx : the seismic catalog of the local seismic network</p> <p>Injection data of N5&amp;N7.xlsx : the injection data of N5 and N7 (with permission of the operator)</p>

opencc-by-4.0Feb 2020View details →
zenodo32/100

A new lithospheric density and magnetic susceptibility model of Iran, starting from high resolution seismic tomography

<p>The Iranian collisional belt formed through&nbsp;different geological events, some of which are still in progress, such as the convergence between Eurasian and Arabian plates,&nbsp;that led to the formation of a complex structure&nbsp;throughout the entire area. To better investigate these structures, we realize a 3D&nbsp;model of the lithosphere in Iran showing the density and the magnetic susceptibility distribution, obtained from a Bayesian joint gravity and magnetic field&nbsp;inversion, starting from a&nbsp;high-resolution seismic tomography (Kaviani et al., 2020).&nbsp;With these models we also calculate the rigidity distribution of the area. The Data Cube uploaded&nbsp;contains the density, magnetic&nbsp;susceptibility and shear modulus volumes, the Bouguer gravity field and the&nbsp;magnetic field, and the Moho, Curie depth and&nbsp;sediment base depth surfaces.</p>

opencc-by-4.0Jun 2023View details →
zenodo32/100

Pre-CSRM: A 3-D seismic model of the shallow crust in continental China

<p>This high-resolution shallow three-dimensional seismic model is constructed&nbsp;for the top 10 km of the upper crust in continental China, based on the&nbsp;constraints of P polarization, Rayleigh wave ellipticity and receiver function obtained from records of <strong>3848</strong> seismic stations&nbsp;during 1990 and 2017. The&nbsp;model has a spatial resolution of 0.3 degree * 0.3 degree in the north-south seismic belt and the trans-north China orogen, and 0.5&nbsp;degree * 0.5&nbsp;degree in the rest of continental China (except the Tarim basin and southwest Tibet with no station coverage). The seismic constraints used for the construction of the model consist of the&nbsp;<strong>5,439,702</strong> polarization angle measurements&nbsp;from the P-wave waveforms of 9361&nbsp;tele-seismic earthquakes, the short-period (4 - 8 s) Rayleigh wave ellipticity estimated from the&nbsp;continuous waveforms of&nbsp;seismic ambient noise, and the stacked receiver functions estimated from&nbsp;<strong>2,125,021</strong> original receiver functions calculated based on&nbsp;the waveforms of 9361 tele-seismic events.&nbsp;Please click on <a href="https://doi.org/10.5281/zenodo.8103561"><strong>link</strong></a> for the datasets.</p> <p>中国大陆区域地壳顶部10 km范围内高分辨率浅层三维地震学模型以从中国大陆区域1990 至 2017 年间 <strong>3848</strong> 个台站原始数据提取的 P 波偏振、瑞利波椭率和接收函数作为约束。该模型在南北地震带和华北造山带区域的空间分辨率为 0.3 度&nbsp;* 0.3 度,在中国大陆其他区域的空间分辨率为&nbsp;0.5 度&nbsp;* 0.5 度&nbsp;(除没有台站覆盖的塔里木盆地和青藏高原西南区域)。构建模型的地震学约束包括从&nbsp;9361 个远震 的 P 波波形测量的&nbsp;<strong>5,439,702 </strong>个偏振角度、从连续背景噪声波形测量的短周期 (4 - 8 s) 瑞利波椭率频散、和利用从 9361 个远震事件提取的 <strong>2,125,021</strong> 条接收函数计算得到的单台叠加接收函数。下载上述数据库请点击<strong><a href="https://doi.org/10.5281/zenodo.8103561">链接</a></strong>。</p> <p><strong>Reference</strong>: Xiao, X., Cheng, S., Wu, J., Wang, W., Sun, L., Wang, X., &amp; Wen, L. (2021). Shallow seismic structure beneath the continental China revealed by P-wave polarization, Rayleigh wave ellipticity and receiver function.&nbsp;Geophysical Journal International,&nbsp;225(2), 998-1019. <strong><a href="https://doi.org/10.1093/gji/ggab022">Paper link</a></strong></p> <p>If you face any problem or issue in the usage of this model, please feel free to communicate with the corresponding author Xiao Xiao (<strong>xiaox.seis@gmail.com</strong>).&nbsp;</p>

opencc-by-4.0Apr 2023View details →
zenodo32/100

Pre-CSRM: An uppermost mantle seismic Pn-velocity in continental China

<p>The&nbsp;uppermost mantle seismic Pn-velocity&nbsp;model is inverted from a new tomographic scheme integrating&nbsp;a&nbsp;combined dataset of 32,427 absolute Pn travel times and 62,431 interstation Pn differential travel times (<a href="https://doi.org/10.1029/2022JB025667">Ma et al., 2023</a>).&nbsp;The model has spatial resolutions of 0.75&deg;&nbsp;&times;&nbsp;0.75&deg;&ndash;1&deg;&nbsp;&times;&nbsp;1&deg; in the north-south seismic belt and 1.5&deg;&nbsp;&times;&nbsp;1.5&deg;&ndash;3&deg;&nbsp;&times;&nbsp;3&deg; in other regions.&nbsp;The combined Pn travel time dataset&nbsp;used for the inversion of the model is selected from <strong>95,878 </strong>Pn travel times manually picked from the recordings of&nbsp;<strong>3,446&nbsp; </strong>seismic stations deployed in and around continental China&nbsp;for a total of <strong>6,787 </strong>seismic events between 1992 and&nbsp;2020. Please click on the <strong><a href="https://doi.org/10.5281/zenodo.8112291">link</a></strong> to download the&nbsp;dataset.</p> <p>中国大陆区域上地幔顶部Pn速度模型是根据整合了32,427个Pn绝对到时和62,431个台站间Pn相对到时的反演方案反演而来。该模型的空间分辨率在南北地震带为0.75&deg;&times;0.75&deg;-1&deg;&times;1&deg;,在其他地区为1.5&deg;&times;1.5&deg;-3&deg;&times;3&deg;。用于模型反演的Pn到时筛选自从部署在中国大陆及其周边地区的<strong>3,446</strong>个地震台站共<strong>6,878</strong>个事件的记录中人工挑选的<strong>95,878</strong>个Pn到时数据库。请点击<strong><a href="https://doi.org/10.5281/zenodo.8112291">链接</a></strong>下载该数据集。</p> <p><strong>Reference</strong>:&nbsp;Ma, J.,&nbsp;Sun, L.,&nbsp;Wang, W.,&nbsp;Wu, J.,&nbsp;Wang, X., &amp;&nbsp;Wen, L.&nbsp;(2023).&nbsp;Uppermost mantle seismic&nbsp;<em>Pn</em>-velocity in continental China and its tectonic implications.&nbsp;<em>Journal of Geophysical Research: Solid Earth</em>,&nbsp;128, e2022JB025667.&nbsp;<a href="https://doi.org/10.1029/2022JB025667">https://doi.org/10.1029/2022JB025667</a></p> <p>If you face any problem or issue when using this model, please feel free to communicate with the corresponding author Jiayu Ma (<a href="mailto:majy18@mail.ustc.edu.cn">majy18@mail.ustc.edu.cn</a> or<a href="mailto: seisbird@gmail.com"> seisbird@gmail.com</a>).</p>

opencc-by-4.0Jul 2023View details →
zenodo32/100

Imaging seismic and aseismic plate coupling with interferometric radar (InSAR) in the Hikurangi subduction zone

<p>Data associated with&nbsp;&#39;Imaging seismic and aseismic plate coupling with interferometric radar (InSAR) in the Hikurangi subduction zone published in GRL.</p>

opencc-by-4.0Jul 2023View details →
zenodo32/100

Seismic waveform data collected at Helheim Glacier between Aug, 2012 and Jun, 2017 (part 1)

<p>&nbsp;Raw seismic waveforms (in miniSEED&nbsp;format) at HEL1 station collected at Helheim Glacier between&nbsp;2012 and 2017 (part 1)</p>

opencc-by-4.0Dec 2023View details →
zenodo32/100

Seismic waveform data collected at Helheim Glacier between Aug, 2012 and Jun, 2017 (part 2)

<p>Raw seismic waveforms (in miniSEED&nbsp;format) at HEL1 station collected at Helheim Glacier between&nbsp;2012 and 2017 (part 2)</p>

opencc-by-4.0Dec 2023View details →
zenodo32/100

The catalog of local seismic events in Pingtong

<p>The catalog of local seismic events in Pingtong</p>

opencc-by-4.0Jul 2023View details →
zenodo32/100

Continuous waveform data and the catalog of local seismic events in Sichuan

<p>Continuous waveform data and the catalog of local seismic events in Sichuan</p>

opencc-by-4.0Jul 2023View details →
zenodo32/100

Revealing Crustal Structure of the Western Philippine Sea Subduction Zone through Seismic, Gravity and Magnetic Joint Inversion Based on Minimum Support Cross-Gradient Coupling

<p>Data contains the synthetic model data and field data.<br> Final model contains the joint and single inverison result.&nbsp;<br> First volum of the data and model represents the location on the profile.</p> <p>Second volum of the model represents the depth of the model, which is all positive.</p> <p>Second volum of the data represent the value of the synthetic data.</p> <p>Rec_obs represents the reflection observed data,fir_tob represents the first arrival travel time observed data, the first and the second volum represents the source number and the receiver number.&nbsp;</p>

opencc-by-4.0Aug 2023View details →
zenodo32/100

Crop of Romney seismic-reflection data volume, offshore the North Island of New Zealand

<p>Crop of Romney seismic-reflection data volume, offshore the North Island of New Zealand&nbsp;(Exploration Database, 2023).</p> <p>SEG-Y header locations<br> Inline 4-byte &ndash; loc: 181<br> Xline 4-byte &ndash; Loc 185<br> X 4-byte &ndash; Loc 73<br> Y 4-byte &ndash; Loc 77</p> <p>CRS<br> New Zealand Map Grid<br> &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;Datum: NZ Geodetic Datum 1949<br> &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;Spheroid: Int 1924<br> &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;PM: Greenwich<br> &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;Meters<br> &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;False Northing 6023150m<br> &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;False Easting 2510000m<br> &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;Long of Natural origin 173 dega<br> &nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;Lat of Natural origin -41 dega</p> <p>Exploration Database (2023). New Zealand Petroleum and Minerals. www.nzpam.govt.nz/maps-geoscience/exploration-database/, February 21, 2023.</p>

opencc-by-4.0Aug 2023View details →
zenodo32/100

High-Pressure Single-Crystal Elasticity of Corundum: Implication for Multiple Seismic Structure of 660-km Discontinuity

<p>Here are the experimental data.</p>

opencc-by-4.0Mar 2023View details →
zenodo32/100

Seismic data and receiver functions from two linear dense nodal array in the southern Chinese Altai region

<p>Seismic data and receiver functions from two linear&nbsp;dense nodal array in the southern Chinese Altai region. All data are&nbsp;arranged by seismic events, and the number before the first dot of each file name represents the station number.</p>

opencc-by-4.0Sep 2023View details →
zenodo32/100

Rupture Jumping and Seismic Complexity in Models of Earthquake Cycles for Fault Stepovers with Off-Fault Plasticity

<p>Fault stepovers are prime examples of geometric complexity in natural fault zones which may affect seismic hazard by determining whether an earthquake rupture continues propagating, or abruptly stops. However, the long-term pattern of seismicity near fault stepovers and underlying mechanisms of rupture jumping in the context of earthquake cycles are rarely studied. Leveraging a hybrid numerical scheme combining the finite element and the spectral boundary integral methods, FEBE, we carry out fully dynamic simulations of Sequences of Earthquakes and Aseismic Slip (SEAS) for both compressive and tensile stepovers, with off-fault plasticity. We consider a rate-and-state friction law for the fault friction, and pressure sensitive Drucker-Prager plasticity for the off-fault bulk response.&nbsp;&nbsp;We observe that the accumulation of plastic deformation, an indication of off-fault damage, is significantly different in the two cases with more plastic deformation projected in the overlapping region for the tensile stepover. The seismic pattern for a tensile stepover is more complex than for a compressive stepover, and incorporating plasticity also increases complexity, relative to the elastic case. A tensile stepover with off-fault plasticity shows rupture segmentation, temporal clustering, and frequent rupture jumping from one fault to another. These results shed light on possible mechanisms of rupture jumping in fault stepovers as well as the long-term evolution of the fault zone.</p>

opencc-by-4.0Sep 2023View details →
zenodo32/100

Output datasets from model for the paper "On the potential role of viscoelasticity in fluid-induced seismicity"

<p>Output datasets from model for &quot;On the potential role of viscoelasticity in fluid-induced seismicity&quot;&nbsp;</p>

opencc-by-4.0Oct 2023View details →
zenodo32/100

Receiver-function datasets of the passive-source seismic profiles in the northeastern Tibetan plateau contributed by LRC

Open the record for dataset details and reuse information.

opencc-by-4.0Aug 2024View details →
ClinicalTrials.gov32/100

A Study to Evaluate the Introduction of New Staffing Models in Intensive Care: a Realist Evaluation (SEISMIC-R)

ClinicalTrials.gov study NCT05917574. IPD Sharing: NO. Countries: 1. Publications: 1.

closedIPD-NOFeb 2026View details →
dryad32/100

Subduction thermal regime, slab dehydration, and seismicity distribution beneath Hikurangi based on 3-D simulations

Open the record for dataset details and reuse information.

publicJun 2017View details →
dryad32/100

Seismic moment rate and recurrence interval of small-size earthquakes from a 3-D perspective

Open the record for dataset details and reuse information.

publicAug 2017View details →

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