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5 results for “Long Valley Caldera”
THD technique applied on Vp data of Long Valley Caldera
<p>We considered the V<sub>p</sub> tomographic model of Seccia et al. (2011) for Long Valley Caldera on which we applied the Horizontal Gradient technique for retrieving geometrical information about the deep structures characterizing the first 10 km of crust. Specifically, after the regularization through spatial based kriging interpolator, we compute the horizontal derivatives on single z-layers with sampling step of 500 m. The results are presented in Gola G., Barone A., Castaldo R., Chiodini G., D'Auria L., Garcia-Hernandez R., Pepe S., Solaro G. & Tizzani P. "A novel multidisciplinary approach for the thermo-rheological study of volcanic areas: The case study of Long Valley Caldera", which has been submitted for possible publication in Journal of Geophysical Research - Solid Earth.</p> <p>Coordinates: North America NAD27 UTM Zone 11N<br> Easting: 308000 - 353000 m.; Northing: 4155000 - 4185000 m; XY resolution: 500 m.</p>
3D attenuation model of Long Valley Caldera (CA)
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3D spatial distribution of the seismic Gutenberg-Richter parameters (a and b values) in Long Valley Caldera
<p>3D distribution of the <em>a</em> and <em>b</em> parameters of the Gutenberg-Richter (GR) law. The analysis is presented in Gola G., Barone A., Castaldo R., Chiodini G., D'Auria L., Garcia-Hernandez R., Pepe S., Solaro G. & Tizzani P. "A novel multidisciplinary approach for the thermo-rheological study of volcanic areas: The case study of Long Valley Caldera", which has been submitted for possible publication in Journal of Geophysical Research - Solid Earth. For this purpose, we used a dataset consisting of more than 220,000 earthquakes from the NCEDC catalogue (NCEDC, 2014), spanning the interval 1978-2017 and located in the surroundings of Long Valley Caldera. We mapped the <em>a</em> and <em>b</em> values for a volume of 50×50×30 km<sup>3</sup>, over a grid of points having a regular spacing of 0.5 km.</p> <p>Coordinates: North America NAD27 UTM Zone 11N<br> Easting: 310000 - 350000 m.; Northing: 4150000 - 4185000 m</p> <p> </p>
Geological model of Long Valley Caldera
<p>Borehole lithostratigraphic data (Table S1) and boundary surfaces (surface_01-05) of Long Valley Caldera 3D geological model. This geological model is used in Gola G., Barone A., Castaldo R., Chiodini G., D'Auria L., Garcia-Hernandez R., Pepe S., Solaro G. & Tizzani P. "A novel multidisciplinary approach for the thermo-rheological study of volcanic areas: The case study of Long Valley Caldera", which has been submitted for possible publication in Journal of Geophysical Research - Solid Earth.</p> <p>Coordinates: North America NAD27 UTM Zone 11N</p> <p>Easting: 311000 - 360000 m.; Northing: 4155000 - 4187000 m; XY resolution: 500 m.</p>
Thermo-Rheological model of Long Valley Caldera
<p>3D Thermo-Rheological models of Long Valley Caldera presented in Gola G., Barone A., Castaldo R., Chiodini G., D'Auria L., Garcia-Hernandez R., Pepe S., Solaro G. & Tizzani P. "A novel multidisciplinary approach for the thermo-rheological study of volcanic areas: The case study of Long Valley Caldera", which has been submitted for possible publication in Journal of Geophysical Research - Solid Earth. We evaluated the temperature distribution and the brittle-ductile values in a volume of 32×50×30 km<sup>3</sup>, along East, North and depth directions, respectively. The optimized solution of the conductive-convective model is evaluated with a reservoir permeability of 5.0·10<sup>−14</sup> m<sup>2</sup>, a fault-zone permeability of 5.0·10<sup>−14</sup> m<sup>2</sup> and a temperature of the magmatic intrusion beneath the caldera of 800°C. The simulated fluid velocity magnitude (mm/year) along x , y and z directions is given positive eastward, northward and upward, respectively. The purely-conductive temperature distribution used as initial condition of the conductive-convective simulation is also given. Finally, we computed the 3D Brittle-Ductile (BD) stratification by considering the optimized conductive-convective thermal model and using a pore fluid factor, a strain rate and a β value equal to 0.36, 1.2, 10<sup>–9</sup> s<sup>–1</sup>, respectively. Further details on the selected petrophysical parameters can be found in the Tables 2 and 3 of the manuscript.</p> <p>The values of the Thermal and Velocity models are gridded with a regular spacing of 0.25 km. The values of the BD model are gridded with a regular spacing of 0.5 km.</p> <p>Coordinates: North America NAD27 UTM Zone 11N</p> <p>Easting: 311000 - 360000 m.; Northing: 4155000 - 4187000 m.</p>
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