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Zircon geochronology is a critical tool for establishing geologic ages and time scales of processes in the Earth's crust.

However, for zircons compromised by open system behavior, achieving robust dates can be difficult.

This has therefore become the principal material used in UPb to yield the radiogenic fractions.

For zircons with very low common Pb contents, an adequate correction may be made by estimating common Pb from a general terrestrial Pb evolution model (e.g.

When compositions yielding such concordant ages are plotted graphically (Fig.

5.4) they define a curve which was termed the concordia by Wetherill (1956a).

After being mounted, the crystals can be analyzed using an instrument such as a SHRIMP (Sensitive High mass Resolution Ion Micro Probe) which focuses a very narrow ion beam onto the grains so that mass spectrometers can measure the ratios of the isotopes vaporized from the targeted spot.

polyphase core–rim structures) and evidence for Pb mobility not linked to discrete crystallization episodes (Pb loss, incorporation of common Pb, high-temperature Pb mobilization).

Interpreting complex U–Pb zircon age data therefore requires imaging of zircon crystals and texturally-controlled sampling to constrain the fine-scale processes affecting the U–Pb zircon systematics.

The concordia curve can be drawn by substituting decay constants and successive values of t into the right-hand sides of equations [5.7] and [5.8], and plotting the results for each value of t.

Pb geochronology, in view of their tendency to incorporate large concentrations of uranium but very little initial (non-radiogenic) lead.

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However, their limited distribution restricts their usefulness.

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