Results 21 to 30 of about 110 (90)
Abstract The majority of geothermal energy is produced in tectonically active volcanic‐arc regions due to their high geothermal gradients. Reservoirs in these settings are often stratified with smectite/kaolinite‐, illite‐, and chlorite‐rich zones, in order of increasing depth and temperature. Eighteen andesitic core and surface samples were taken from
Barnaby Fryer +7 more
wiley +1 more source
Abstract Natural radiogenic isotopes (primarily 87Sr/86Sr) from hot springs in the Upper Geyser Basin of the Yellowstone Plateau volcanic field and associated rocks were used to evaluate groundwater flow patterns, water‐rock reactions, and the extent of mixing between various groundwater sources.
James B. Paces +4 more
wiley +1 more source
Paleoseismology of the southwestern Morelia-Acambay fault system, central Mexico [PDF]
Fr The Morelia-Acambay Fault System (MAFS) consists of a sequence of E-W and NNE-SSW trending normal faults within the Trans-Mexican Volcanic Belt.
V. H. Garduño Monroy et al
doaj
Hydrothermal alteration at Los Azufres geothermal held is mostly propylitic showing progressive dehydration with depth, and temperature increase. The evolution of this system is inferred to be related to deep liquid water, boiling when ascending through fractures connected to the surface.
E González-Partida +2 more
openaire +1 more source
Acidophilic sulphate‐reducing bacteria: Diversity, ecophysiology, and applications
Acidophilic sulphate‐reducing bacteria (aSRB) perform dissimilatory sulphate reduction under low pH and high metal conditions. They play key roles in the sulphur and carbon cycles in natural acidic environments, emphasized by their interactions with other microbial groups, which create an intricate ecological network. Potential applications of aSRB and
Luis Felipe Valdez‐Nuñez +4 more
wiley +1 more source
Hydrothermal geochemical signatures in outcropping rock samples of the super‐hot Los Humeros geothermal field were discovered by using an integrated geochemometric study of the mobility of components (major oxides) and trace elements. Chemical component and element mobilities were determined by using the Gresens–Grant equation for mass balances.
D. Yáñez-Dávila +7 more
wiley +1 more source
La clasificación basada en el índice de exergía específica (SExI) propuesta por Lee (Lee, K.C., 1996, Proceedings, Twenty-First Workshop SGP-TR-151 on Geothermal Reservoir Engineering: Stanford, California, Stanford University, 85-92; Lee, K.C., 2001, Geothermics, 30(4), 431-442) ha sido escasamente utilizada en las ciencias geológicas como una manera ...
Hipólita Ramajo +5 more
openaire +2 more sources
Abstract We present a combined mineralogical, chemical, and Sr-Nd isotopic study of hydrothermal alteration effects in near-surface Pleistocene rhyolite sampled at two distinct localities from the Los Azufres geothermal field (LAGF), Mexico. The alteration mineralogy of the near-surface rocks is dominated by silica polymorph minerals (cristobalite ...
Surendra P. Verma +3 more
openaire +2 more sources
To investigate the effects of hydrothermal alteration on the chemistry of volcanic rocks, we analyzed the whole rock chemical composition (major and trace elements, including rare-earth elements – REE) of two distinct portions of a drill well core sample
Ignacio S. Torres-Alvarado +3 more
doaj
La clasificación basada en el índice de exergía específica (SExI) propuesta por Lee (Lee, K.C., 1996, Proceedings, Twenty-First Workshop SGP-TR-151 on Geothermal Reservoir Engineering: Stanford, California, Stanford University, 85-92; Lee, K.C., 2001 ...
Hipólita Ramajo +5 more
doaj

