Federal government websites often end in. Geochronology-based studies of sediment provenance typically rely on dating n ≈ – single detrital zircon crystals from individual. Disruption of the original crustal architecture as a result of tectonic events often complicates studies of the crustal evolution of Precambrian cratons.
William A. While sandstone petrography continues to provide unique information about provenance, more recently, detrital-zircon geochronology has. Geology ; 46 11 : —
Detrital zircon geochronology is the science of analyzing the age of zircons deposited within a specific sedimentary unit by examining their inherent radioisotopesmost commonly the uranium—lead ratio. Detrital zircon geochronology is rapidly developing into an essential tool in Earth science research because (Volume publication date May ). The full text of this article hosted at iucr.
Copyright remains with the author s or their institution s. Permission for reuse free in most cases can be obtained from RightsLink. Based on research of the petrology, geochemistry, and zircon U—Pb dating of detrital rocks in the Late Triassic Wenbinshan Formation in southwestern Fujian, and comparing the detrital zircon ages of Wenbinshan Formation with those of Late Paleozoic — Early Mesozoic main basins in South China, the sedimentary provenance of the Late Triassic in southwestern Fujian and its implications for changes in basin properties are discussed.
International Journal of Earth Sciences. Detrital zircon dating and tracing the provenance of dinosaur bone beds from the Late Cretaceous Wangshi Group in Zhucheng, Shandong, East China.
U–Pb dating on inherited detrital zircons has been applied to obtain the probable maximum age of deposition of the detrital protolith of the.
Our primary geochronological service is detrital zircon U-Pb geochronology. We also offer bespoke dating of other mineral-isotope systems that may provide.
The hundreds of published studies utilizing detrital zircon in the last 20 Detrital zircon U-Pb dating and Hf isotope study of late Palaeozoic.