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7 results for “Los Humeros”
P-S waves 3D velocity model of Los Humeros area from earthquake based travel-time tomography using CAT3D software (OGS)
<p>The dataset contains the 3D velocity model (VP (m/s), VS (m/s) and VP/VS) obtained from the tomographic inversion of seismological data in the area of Los Humeros (Mexico). The model was performed in the frame of the GEMex project (Mexico‐Europe Cooperation for research of enhanced geothermal systems and super-hot geothermal systems, WP5 ‘Detection of deep structures’, Jousset et al., D5.3, 2019).</p> <p>The inversion used 2661 P arrivals and 2272 S arrivals associated to 395 earthquakes recorded by 37 stations. The picking data was provided by Toledo et al., 2019.</p> <p>The inversion was performed by CAT3D software, a tomographic tool developed by OGS, which uses the SIRT method (Simultaneous Iterative Reconstruction Technique, Stewart, 1993) as inversion algorithm and the ray tracing procedure based on minimum time principle (Böhm et al., 1999). The velocities used as initial model for tomography were provided by the interpolated values obtained from the velocity analysis of four 2D seismic lines acquired inside the same investigated area by the tomographic inversion (See GEMex deliverable D5.3).</p> <p>The 3D velocity model is defined by a 3D grid of 61 nodes in X, 69 nodes in Y and 29 nodes in Z, equally spaced by 250 m in all directions. The total dimensions of the model is 15x17x7 km and the borders positions are (m) (WGS 84/UTM ZONE 14N):</p> <p>Xmin = 655000, Xmax = 670000</p> <p>Ymin = 2168000, Ymax = 2185000</p> <p>Zmin = -3000, Zmax = 4000</p>
3D resistivity structure of the Los Humeros geothermal field.
<p>The dataset is the final three-dimensional resistivity model of the high temperature geothermal field Los Humeros, in Mexico.</p> <p>The model is described in deliverable 5.2 of the GEMex Project, funded by the European Union’s Horizon 2020 research and innovation programme under grant agreement No. 727550, and by the Mexican Energy Sustainability Fund<br> CONACYT-SENER, Project 2015-04-268074.</p>
3D density models of the Los Humeros and Acoculco geothermal fields, Mexico.
<p>The GEMex project addresses different challenges in the development of Enhanced Geothermal Systems (EGS) and Superhot Geothermal Systems (SHGS) in the Trans-Mexican Volcanic Belt. Although they are located in similar tectonic settings, the geothermal conditions in Acoculco and Los Humeros differ and they can be categorized as an EGS and a SHGS system, respectively. The Los Humeros field is currently under conventional exploitation. North of the current production area, temperatures higher than 380°C are expected. The Acoculco site presents temperatures >300°C at a depth of 2 km, but a reservoir has not been identified. The main goal of this work is to visualize and characterize the reservoir conditions using gravity data. To accomplish this, we processed data from a total of 344 gravity stations at Los Humeros and 84 stations at Acoculco. The datasets contain the 3D density model of the Los Humeros and Acoculco geothermal fields as density contrasts values in g/cm³. The background density is 2.67 g/cm³.</p>
Magneto-telluric data from the Los Humeros geothermal field in Mexico: time series and edi-files
<p>The data are from the Los Humeros geothermal field in Mexico.</p> <p>The dataset is composed of time series of magneto-telluric data and edi-files obtained from the time series. A file containing the location of the soundings and calibration files are also in the dataset.</p> <p>The Metronix equipment was used to acquire the data.</p> <p>The data were gathered under the European Union’s Horizon 2020 research and innovation programme under grant agreement No. 727550, and by the Mexican Energy Sustainability Fund CONACYT-SENER, Project 2015-04-268074.</p>
Transient Electromagnetic data from the Los Humeros geothermal field in Mexico: raw data
<p>The dataset is composed of raw data from TerraTEM (from Monex GeoScope, single loop) from the Los Humeros geothermal field, Mexico and their locations in a .csv file.</p> <p>The data were gathered under the European Union’s Horizon 2020 research and innovation programme under grant agreement No. 727550, and by the Mexican Energy Sustainability Fund CONACYT-SENER, Project 2015-04-268074.</p>
Thermal model of the Los Humeros super-hot geothermal system, Mexico
<p>The dataset contains 3D thermal model (format - .vtk and .h5) of Los Humeros geothermal system at a local scale (extent defined in Calcagno et al., 2018). The boundary conditions used for this thermal model are obtained from Scenario 3b of regional model discussed in<strong> </strong>EU Deliverable D6.3<strong> </strong>(<a href="http://doi.org/10.5281/zenodo.3723039">10.5281/zenodo.3723039</a>) and D6.6 (<a href="https://doi.org/10.5281/zenodo.3723224">10.5281/zenodo.3723224</a>).</p> <p>Before using the results of the model, the user is advised to carefully read the model parameters, assumptions and uncertainties associated with the model as reported in Deliverable D6.3 and Deliverable D6.6.</p> <ol> <li>The .h5 file contains data and attributes (quantity, unit)</li> <li>The .vtk files contains the following information <ul> <li>x, y, z UTM coordinates (m)</li> <li>temp Temperature (°C)</li> <li>head Hydraulic head (m)</li> <li>pres Pressure (MPa)</li> <li>por Porosity (-)</li> <li>q Heat flow (W m<sup>-2</sup>)</li> <li>kx, ky, kz Permeability (m<sup>2</sup>)</li> <li>vx, vy, vz Specific discharge or Darcy velocity (m s<sup>-1</sup>)</li> <li>lx, ly, lz Thermal conductivity (W m<sup>-1</sup> K<sup>-1</sup>)</li> </ul> </li> </ol> <p>Additional information regarding the model is presented in the PDF document.</p>
MT_Data-LOS-HUMEROS
<p>We put forward our EDI data used in our manuscript DEEP STRUCTURAL MODEL OF LOS HUMEROS AND RESURGENT LOS POTREROS CALDERAS FROM MAGNETOTELLURIC SOUNDINGS. We also added the 6 figures that are part of this work.</p>
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