Results 51 to 60 of about 100 (67)
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Geothermics, 1990
A simulation of the temperature field underlying Los Humeros caldera is obtained through numerical solution of the energy-conservation equation for a conductive heat flow process. The up-date information on geological, geochemical, geophysical and geochronological studies is used to estimate the parameters of the internal structure of the caldera.
Surendra P Verma
exaly +2 more sources
A simulation of the temperature field underlying Los Humeros caldera is obtained through numerical solution of the energy-conservation equation for a conductive heat flow process. The up-date information on geological, geochemical, geophysical and geochronological studies is used to estimate the parameters of the internal structure of the caldera.
Surendra P Verma
exaly +2 more sources
Bulletin of the Geological Society of America, 2012
Los Humeros is the largest caldera volcano in the Mexican volcanic belt. Its second largest caldera-forming eruption, the ca. 0.1 Ma Zaragoza eruption, is recorded by two Plinian pumice-fall layers and a zoned intra-Plinian ignimbrite. Diverse pumice types within the ignimbrite provide insights about the way that different magmas within a single ...
Gerardo Carrasco-Núñez +2 more
exaly +2 more sources
Los Humeros is the largest caldera volcano in the Mexican volcanic belt. Its second largest caldera-forming eruption, the ca. 0.1 Ma Zaragoza eruption, is recorded by two Plinian pumice-fall layers and a zoned intra-Plinian ignimbrite. Diverse pumice types within the ignimbrite provide insights about the way that different magmas within a single ...
Gerardo Carrasco-Núñez +2 more
exaly +2 more sources
Seismic models of the Los Humeros caldera (Mexico) using the GEMEX project data
2020<p>In the framework of the GEMEX project (cooperation between Europe and Mexico for geothermal development), a dense network of 45 stations was deployed in 2017-2018 in the Los Humeros caldera, Mexico.</p><p>Thanks to this network an intense local seismic activity has been recorded in the geothermal ...
Marco Calò +8 more
openaire +1 more source
International Geology Review, 2009
We present results of our simulation study of the effects of the depth (top of the magma chamber at 5–10 km) and volume (1000–1400 km3) of the primary heat source beneath the Los Humeros caldera. The thermal gradient in the vicinity of the magma chamber calculated from the temperature excess (difference between the simulated and the initial ...
Surendra P. Verma +2 more
openaire +1 more source
We present results of our simulation study of the effects of the depth (top of the magma chamber at 5–10 km) and volume (1000–1400 km3) of the primary heat source beneath the Los Humeros caldera. The thermal gradient in the vicinity of the magma chamber calculated from the temperature excess (difference between the simulated and the initial ...
Surendra P. Verma +2 more
openaire +1 more source
SEG Technical Program Expanded Abstracts 1983, 1983
Los Humeros caldera is a Quaternary volcanic structure located on the eastern portion of the Mexican volcanic belt. Geothermal exploration, including well drilling, is presently carried out; geophysical surveys over the 200 km’ structure include aeromagnetometry, gravimetry, tellurics, self-potential, resistivity soundings (Schlumberger).
openaire +1 more source
Los Humeros caldera is a Quaternary volcanic structure located on the eastern portion of the Mexican volcanic belt. Geothermal exploration, including well drilling, is presently carried out; geophysical surveys over the 200 km’ structure include aeromagnetometry, gravimetry, tellurics, self-potential, resistivity soundings (Schlumberger).
openaire +1 more source
The Los Humeros (Mexico) geothermal field model deduced from new geophysical and geological data
Geothermics, 2018Fernando Corbo-Camargo +2 more
exaly

