The chronologic record encoded in accessory minerals, based on the radioactive decay of U
and Th, is indispensable to extract quantitative process rates over timescales encompassing …

The combination of U-Th disequilibrium/U-Pb and (U-Th)/He dating of zircon (ZDD) has
provided a relatively new radiometric approach suitable for dating Quaternary zircon …

Longevity and size of magmatic systems are fundamental factors for assessing the potential
of a geothermal field. At Los Humeros volcanic complex (LHVC), the first caldera‐forming …

We have measured 238 U–206 Pb, 235 U–207 Pb, and 232 Th–208 Pb ages on Quaternary
zircons by laser ablation, single-collector, magnetic sector inductively coupled plasma mass …

Based on a detailed geological map and stratigraphy aided by new 230 Th/238 U and 206
P/238 U age determinations we established the eruptive chronology of the Tres Vírgenes …

Detailed volcano-stratigraphy and 40 Ar/39 Ar dating are used for the first time to reconstruct
the eruptive evolution of the Alchichica maar and to contribute to the understanding of maar …

The recognition of past climatic fluctuations in sedimentary sequences in central Mexico is
relevant for understanding the forcing mechanisms and responses of climatic system in the …

The origin, evolution and long-term preservation of andesitic continents within the context of
destructive plate boundaries are still enigmatic for geoscientists. Here we use U single bond …

The intermontane Serdán-Oriental basin (SOB), located in the Trans-Mexican Volcanic Belt,
records a highly contrasting volcanic field with nearly 166 monogenetic volcanoes, including …

In situ small‐spot U‐Pb geochronology is essential for measuring zircon crystals containing
micrometre‐scale heterogeneities, abundant inclusions, inevitable cracks and narrow …