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35 results for “Crustal Structure”
Data for "Crustal Structure Constraints From the Detection of the SsPp Phase on Mars"
<p>This file contains the event data for eight marsquakes used in the paper entilted "Crustal Structure Constraints From the Detection of the SsPp Phase on Mars" for publication in Earth and Space Science.</p>
Supplemental Datafiles for the manuscript "Crustal structure of northern Borneo from VDSS: Implications for subduction termination and the tectonic reconstruction of SE Asia"
<p>Processed waveform data (windowed/filtered) from the seismic stations for the Virtual Deep Seismic Sounding (VDSS) study in northern Borneo.</p>
Crustal Structure of the Yunnan, China Region Revealed by Adjoint Inversion of Frequency-dependent Traveltimes
<p>These files are observed waveforms used in the paper entitled 'Crustal Structure of the Yunnan, China Region Revealed by Adjoint Inversion of Frequency-dependent Traveltimes' by Wei et al. (2024).</p>
Datasets related to paper "Crustal structure and fault geometries of the Garhwal Himalaya, India: Insight from new high-resolution gravity data modeling and PSO inversion"
<p>The files include Satellite gravity data, topography and earthquake data used in the paper "Crustal structure and fault geometries of the Garhwal Himalaya, India: Insight from new high-resolution gravity data modeling and PSO inversion" by Chamoli A., Rana S., Dwivedi D., Pandey A.K.. This has been submitted to Journal of Geophysical Research: Solid Earth. Restrictions applied to the availability of the land gravity data set.</p>
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. <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. </p>
Data from: Ambient noise tomography of upper crustal structures and Quaternary faults in the Seoul metropolitan area and its geological implications
<p class="0"><span><span><span>We investigate the upper-crustal seismic velocity structure in the Seoul metropolitan</span> <span>area, where about 20 million people live. The Chugaryeong fault zone (CFZ) is</span> <span>placed in this area, but the seismic hazard potential remains unclear. We conducted</span> <span>ambient noise tomography to illuminate the high-resolution upper-crustal structure</span> <span>in the Seoul metropolitan area. We analyzed continuous vertical seismic records</span> <span>for ~5 months from a dense seismic array with 77 broadband stations. Group</span> <span>velocity dispersion curves and tomographic maps were extracted between 0.5 and 10</span> <span>s periods. We inverted 3-D group velocity tomography models up to a depth of ~10</span> <span>km from the group velocity maps. The shear-wave velocity model is consistent with</span> <span>the geological features. High-velocity anomalies at shallow depths are correlated</span> <span>with the surface topography and geology. The CFZ is located at a low velocity below the 5 km depth and presented as the simplified model. The large </span><span>V</span><span><sub>S</sub> </span><span>contrast</span> <span>regions are located beneath NS-trending faults. The cross-sections coincide with</span> <span>the near-vertical strike-slip faults in this area. In the southern region of the Seoul</span> <span>metropolitan area, low-velocity anomalies correlate with high heat flow regions. Our</span> <span>results effectively suggest high resolution upper-crustal structures and subsurface</span> <span>hidden faults in the urban area.</span></span></span></p>
Supplemental Datafiles for the manuscript "Crustal structure of northern Borneo from VDSS: Implications for subduction termination and the tectonic reconstruction of SE Asia"
<p>Processed waveform data (windowed/filtered) from the seismic stations for the Virtual Deep Seismic Sounding (VDSS) study in northern Borneo.</p>
Dataset:Ray and Halo impact craters on Ganymede : fingerprint for decoding Ganymede´s crustal structure
<p>The geological basemap used in the study is from Kersten et al., 2021. </p>
Crustal and upper mantle structure beneath SE China from joint analysis of receiver functions and Rayleigh-wave dispersion
<p>This file contains our new 3-D shear-wave velocity model for SE China.</p>
Impact of Ancient Tectonics on Intracontinental Deformation Partitioning: Insights from Crustal Structures of the Chinese Altai Mountains
<p>The dataset includes all recevier functions (SAC format files) used in this study.</p>
Data from: Ambient noise tomography of upper crustal structures and Quaternary faults in the Seoul metropolitan area and its geological implications
Open the record for dataset details and reuse information.
POTENTIAL FIELDS MODELING FOR THE CAYOS BASIN (WESTERN CARIBBEAN PLATE): IMPLICATIONS IN BASIN CRUSTAL STRUCTURE
<p>DATA SET FOR: POTENTIAL FIELDS MODELING FOR xcxcTHE CAYOS BASIN (WESTERN CARIBBEAN PLATE): IMPLICATIONS IN BASIN CRUSTAL STRUCTURE.</p> <p>Data description: These data correspond to the geophysical dataset (gravimetric and magnetic) of the Cayos Basin obtained by the Colombian National Hydrocarbon Agency (ANH) and the U.S. Geological Survey (USGS). Bathymetric information was obtained from the ETOPO datasets from the National Oceanic and Atmospheric Administration (NOAA).</p>
Seismic crustal structure of the North China Craton and surrounding area: Synthesis and analysis
<p>Nccrust is a new digital model (NCcrust) of the seismic crustal structure of the Neoarchean North China Craton (NCC) and its surrounding Paleozoic-Mesozoic orogenic belts (30–45∘N, 100–130∘E).</p> <p>All available seismic profiles, complemented by receiver function interpretations of crustal thickness, are used to constrain a new comprehensive crustal model NCcrust.</p> <p>The model, presented on a 0.25∘ × 0.25∘grid, includes the Moho depth and the internal structure (thickness and velocity) of the crust specified for four layers (the sedimentary cover, upper, middle, and lower crust) and the Pn velocity in the uppermost mantle.</p> <p>Xia, B., Thybo, H. & Artemieva, I. M. Seismic crustal structure of the North China Craton and surrounding area: Synthesis and analysis. J. Geophys. Res.-Solid Earth 122, 5181-5207, doi:10.1002/2016jb013848 (2017).</p> <p>Any questions or requests, please has no hesitation in email me: bingxia0127@gmail.com</p>
Mars's crustal and volcanic structure explained by southern giant impact and resulting mantle depletion
<p>Data to recreate relevant figures for the manuscript "Mars’s crustal and volcanic structure explained by southern giant impact and resulting mantle depletion".</p>
Data used in paper "Crustal structure across the extinct mid-ocean ridge ..."
<p>Seismograms are used for generating receiver functions for 11 OBS in the Central sub-basin of the SCS. We note that seismograms are windowed to include only the P wave (40 s and 60 s before and after the predicted arrivals). </p> <p>Note: This dataset can only be downloaded to verify the RF results. it can not be used for other seismic applications since it has already been allocated to specific groups that are working on seismic tomography, anisotropy, noise analysis, microearthquake relocations, and waveform modeling. Please contact us at: tyang@sustech.edu.cn for more information. </p>
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