U-pb dating of zircon by la-icp-ms

u-pb dating of zircon by la-icp-ms

The limited Silurian to Early Devonian detrital ages that contrast with the more significant Middle to Late Devonian zircons that document the erosion of contemporaneous magmatic sources formed after a late Silurian to Early Devonian reduction on the magmatic activity along the proto-Andean margin.

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A total of detrital zircon grains from six Wedington samples were recovered for U—Pb detrital zircon geochronological analysis.

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The stratigraphic time interval and the stratigraphic division of the Yanchang Formation has been highly debated with estimates ranging from Middle Triassic to Late Triassic.


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These include Langmuir-probe analysis for the characterization of localized space and floating potentials and ion-kinetic-energy determinations to enhance understanding of the expansion that occurs as a plasma is sampled into a mass spectrometer.

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Description: The origin, extent and timing of intraplate contraction in Patagonia are among the least understood geological processes of southern South America. Our data indicate the presence of a nearly complete Cenozoic record, which refutes previous interpretations of a hiatus during the middle Eocene—late Oligocene in the Central Patagonian Andes.

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