Results 131 to 140 of about 179 (154)
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Naturally occurring heavy radioactive elements in the geothermal microcosm of the Los Azufres (Mexico) volcanic complex

Journal of Environmental Radioactivity, 2015
The Los Azufres geothermal complex of central Mexico is characterized by fumaroles and boiling hot-springs. The fumaroles form habitats for extremophilic mosses and ferns. Physico-chemical measurements of two relatively pristine fumarolic microcosms point to their resemblance with the paleo-environment of earth during the Ordovician and Devonian ...
W A, Abuhani   +9 more
openaire   +2 more sources

Application of the Gauss theorem to the study of silicic calderas: The calderas of La Primavera, Los Azufres, and Los Humeros (Mexico)

Journal of Volcanology and Geothermal Research, 2005
Abstract We explored applications (including limitations) of Gauss's theorem to the study of silicic calderas. First it enables us to determine the mass deficiency from calderas. Mass deficiency itself has also other potential applications. It enables to make qualitative comparisons between calderas. We can use the mass deficiency to test, in a quick
J.O. Campos-Enríquez   +4 more
exaly   +2 more sources

Environmental Impact by Spill of Geothermal Fluids at the Geothermal Field of Los Azufres, Michoacán, Mexico

Water, Air, and Soil Pollution, 2000
Monitoring of surface water and shallow aquifers inside and outside of the Los Azufres geothermal fieldduring the period November 1994 to May 1996 led to thedetection of some contamination of surface water andshallow aquifers due to exploitation of the deepbrines.
P. Birkle, B. Merkel
openaire   +1 more source

Geochemistry of boron in fluids of Los Humeros and Los Azufres hydrothermal systems, Mexico.

2010
Separated water from geothermal wells of high-temperature geothermal fields Los Humeros and Los Azufres in Mexico are unusually rich in boron. According to the isotopic composition, boron in both fields has magmatic origin. Since the Los Humeros fluids, in contrast to Los Azufres, do not show any correlation between B and Cl and have Cl/B ?
RomeroBernard R, Taran Y, Pennisi M
openaire   +2 more sources

Hydro-geochemical and isotopic fluid evolution of the Los Azufres geothermal field, Central Mexico

Applied Geochemistry, 2005
Abstract Hydrothermal alteration at Los Azufres geothermal field is mostly propylitic with a progressive dehydration with depth and temperature increase. Argillic and advanced argillic zones overlie the propylitic zone owing to the activity of gases in the system. The deepest fluid inclusions (proto-fluid) are liquid-rich with low salinity, with NaCl
E. González-Partida   +8 more
openaire   +1 more source

The origin of reservoir fluids in the geothermal field of Los Azufres, Mexico — isotopical and hydrological indications

Applied Geochemistry, 2001
Abstract The calculation of hydrological balance resulted in a potential, average annual infiltration rate of 446±206 mm/m 2 for the Los Azufres geothermal area, which corresponds to a total of 82×10 6 m 3 per a. Due to the highly fractured and faulted structure of the volcanic formations, a considerable potential for the infiltration of recent ...
Peter Birkle   +3 more
openaire   +1 more source

Late Pleistocene rhyolitic explosive volcanism at Los Azufres Volcanic Field, central Mexico

2012
Abstract Los Azufres Volcanic Field hosts the second most important geothermal field of Mexico, with a production of 188 MW of electricity. Based on fieldwork and new geochronological data (14C and 40Ar/39Ar) we define that activity at Los Azufres Volcanic Field started some 1.5 Ma with the emission of basaltic to rhyolitic lavas, and ...
José Luis Arce   +8 more
openaire   +1 more source

Los Azufres geothermal field, Michoacán

2015
G. H. Huitrón R.   +7 more
openaire   +1 more source

Evolution of the geothermal fluids at Los Azufres, Mexico, as traced by noble gas isotopes, δ18O, δD, δ13C and 87Sr/86Sr

Journal of Volcanology and Geothermal Research, 2013
Daniele L Pinti   +2 more
exaly  

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