Results 31 to 40 of about 100 (67)
Compositional zonation in ignimbrites is relatively common, and is often inferred to record gradual withdrawal by an eruption of a density-stratified magma chamber (with silicic magma towards the top and more dense, mafic magma at the bottom). We show that this model does not match observations at the ca.
Gerardo Carrasco-Núñez +2 more
openaire +1 more source
Abstract Studying the behavior of dormant volcanoes is a major challenge in volcanology. Here, we conducted a 10‐year survey of hydrothermal mineralization at Campi Flegrei, an active volcano near Naples in Italy, which last erupted in 1538. Our survey revealed a significant output of boric acid at the hydrothermal sulfate discharge area of Pisciarelli,
M. Piochi +3 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
Se presentan los resultados de un modelado térmico de la cámara magmática subyacente a la caldera de Los Humeros, situada en la parte oriental del Cinturón Volcánico Mexicano.
J. Castillo Román +2 more
doaj +1 more source
The use of the subsurface and the exploitation of subsurface resources require prior knowledge of fluid flow through fracture networks. For nuclear waste disposal, for the enhancement of hydrocarbon recovery from a field, or the development of an ...
Baptiste Lepillier +5 more
doaj +1 more source
Interpretación tridimencional de datos magnetotelúricos en la Caldera de los Humeros, Pue.
N ...
openaire +1 more source
Estimating the depth and evolution of intrusions ar resurgent calderas: Los Humeros (Mexico)
openaire +1 more source
Modelo tridimensional de la caldera de los humeros; implicaciones geológicas y geotérmicas
openaire +1 more source

