Detrital zircon geochronology is rapidly develo** into an essential tool in Earth science
research because of the widespread occurrence of zircon in sedimentary systems; the wide …

Constraining the timing of emplacement, duration and magma extrusion rates of large
igneous provinces is essential for evaluating their petrogenetic evolution and possible links …

Zircon U–Pb geochronology has become a keystone tool across Earth science, arguably
providing the gold standard in resolving deep geological time. The development of rapid in …

Impact glasses found in lunar soils provide a possible window into the impact history of the
inner solar system. However, their use for precise reconstruction of this history is limited by …

Detrital zircon data have recently become available from many different portions of the
Tibetan–Himalayan orogen. This study uses 13,441 new or existing U‐Pb ages of zircon …

The increase in detrital geochronological data presents challenges to existing approaches
to data visualization and comparison, and highlights the need for quantitative techniques …

Detrital geochronology and thermochronology have emerged as primary methods of
reconstructing the tectonic and surficial evolution of the Earth over geological time …

Interpreting the wealth of new data derived from the diverse suite of modern single-grain
provenance approaches available to a sedimentologist requires a thorough understanding …

We determined U-Pb ages for detrital zircons from 26 samples of Paleozoic sandstone from
the Grand Canyon. Cambrian strata yield mainly ca. 1.44 and 1.7–1.8 Ga ages that indicate …

Detrital zircon U–Pb geochronology is a staple of sedimentary provenance analysis and
crustal evolution studies. Constructing detrital age spectra is straightforward for concordant …