RIGOROUS TEMPORAL FRAMEWORKS

RIGOROUS TEMPORAL FRAMEWORKS

for deepened geological context

for deepened geological context

We work with you to develop an approach that matches your project

Geochronological Services

Perhaps you want to elevate your geological study by refining the temporal context?

Or maybe you are designing a
high-impact multidisciplinary study requiring detailed geochronology?

Whatever your needs, we tailor our services to support excellent outcomes for your project

If you are just looking for a short written context piece to accompany an article or funding application, you may be interested in our Publication Support services

The Project Workflow

We can lead or advice on geochronological aspects for one, all, or any combination of these stages within your project

Our Specialty

Applications include:

  • Tephra (volcanic ash) dating for precise depositional ages in sedimentary successions

  • Igneous emplacement ages and tectonic reconstruction

  • Detrital zircon provenance and maximum depositional
    age studies

  • Mineralisation and metamorphic event chronologies

We partner with world-class analytical facilities to conduct radioisotope analysis on a wide variety of mineral systems with specific expertise in uranium-lead dating of zircon

Ready to get started? Reach out to discuss options for your project

Pricing and Payment

Our tailored services come with tailored quotes

Pricing for our services depends on scope, complexity, and analytical costs. We will prepare a custom quote for you based on information provided when you first reach out.

For larger projects, we will arrange a complementary virtual meeting to discuss details before preparing the quote. Fees are separated into consultation and laboratory charges.

New Client Offer!

We are expanding our capabilities in 2026 and to celebrate new partnerships
we are proud to offer

50% off consultation fees

for all new clients, regardless of project scale or complexity

This is particularly relevant to CA-ID-TIMS analyses which can yield analytical precision comparable to, or much less than, zircon crystallisation distributions. In cases where the degree of date variance is greater than analytical uncertainty, a Bayesian eruption / crystallisation age prediction may be more appropriate than a simple weighted mean age.

We facilitate co-analysis of U-Pb isotopes and trace element signatures of zircon to interpret the geochemistry of source terranes. A common application is analysis of stream sediments for interpreting potential porphyry sources in the watershed
(e.g., PIZ - Porphyry Indicator Zircons; Carrasco-Godoy et al., 2024).

To ensure rigor, robustness, and reproducibility, our age-stratigraphic models are constructed based on the modifiedBchron deeptime-specific approach of Traylor et al. (2020) derived from Haslett & Parnell (2008)

Repeat age analysis to corelate tephra outcrops with sufficient confidence can be unnecessarily expensive. Instead, we can coordinate tephrostratigraphic correlation based on zircon characterization.

Depending on available age constraints, we can apply a Bayesian statistical approach to predicting stratigraphic ages throughout a measured sedimentary section

Interested in geochemical signatures for provenance interpretation or mineralization vectoring?

Looking to define ages for specific features within a sedimentary succession?

Geochemical Tephrostratigraphy

Did your magmatic samples yield a complex zircon date distribution?

Interpretation of Zircon Crystallisation

Bchron Age-Stratigraphic Models

Coupled U-Pb and Trace Elements

Advanced Capabilities

As well as excelling in standard geochronological practices, we are at the forefront of technical capabilities with respect to several key applications

Bchron Age-Stratigraphic Models

Looking to define ages for specific features within a sedimentary succession?

Geochemical Tephrostratigraphy

Depending on available age constraints, we can apply a Bayesian statistical approach to predicting stratigraphic ages throughout a measured sedimentary section

To ensure rigor, robustness, and reproducibility, our age-stratigraphic models are constructed based on the modifiedBchron deeptime-specific approach of Traylor et al. (2020) derived from Haslett & Parnell (2008)

Zircon ideal for geochemical tephrostratigraphy >>

Coupled U-Pb and Trace Elements

Interested in geochemical signatures for provenance interpretation or mineralization vectoring?

We facilitate co-analysis of U-Pb isotopes and trace element signatures of zircon to interpret the geochemistry of source terranes. A common application is analysis of stream sediments for interpreting potential porphyry sources in the watershed
(e.g., PIZ - Porphyry Indicator Zircons; Carrasco-Godoy et al., 2024).

Have abundant tephra horizons in your field area that require precise correlation?

Repeat age analysis to corelate tephra outcrops with sufficient confidence can be unnecessarily expensive. Instead, we can coordinate tephrostratigraphic correlation based on zircon characterization.

Depending on the magmatic context of the tephra, analyses may include melt inclusion geochemistry, hafnium isotope ratios, trace element composition, and even crystal morphotype mapping.

In specialized cases, we explore the significance of protracted zircon saturation relative to statistically appropriate age calculations, following the approach of Keller et al. (2018).

This is particularly relevant to CA-ID-TIMS analyses which can yield analytical precision comparable to, or much less than, zircon crystallisation distributions. In cases where the degree of date variance is greater than analytical uncertainty, a Bayesian eruption / crystallisation age prediction may be more appropriate than a simple weighted mean age.

Depending on the magmatic context of the tephra, analyses may include melt inclusion geochemistry, hafnium isotope ratios, trace element composition, and even crystal morphotype mapping.

In specialized cases, we explore the significance of protracted zircon saturation relative to statistically appropriate age calculations, following the approach of Keller et al. (2018).

Example Bchron model from Yuleridge et al. illustrating a model >>
age curve with uncertainty, and model ages for fossil localities (red) >>

Have abundant tephra horizons in your field area that require precise correlation?

Interpretation of Zircon Crystallisation

Did your magmatic samples yield a complex zircon date distribution?

Ready to work together?

Reach out with a description of your project and we can explore options

Want to know more?

See our Frequently Asked Questions page to explore more about our services