Not sure which method suits your sample? Let our experts recommend the most appropriate dating technique based on your material and scientific question.
Not sure which method suits your sample? Let our experts recommend the most appropriate dating technique based on your material and scientific question.
Unsure which isotopic tool can best fingerprint your rock or mineral? We provide customised guidance for source identification and material characterisation.
Unsure which isotopic tool can best fingerprint your rock or mineral? We provide customised guidance for source identification and material characterisation.
High-precision dating of uranium-bearing minerals including zircon, monazite, baddeleyite, titanite, rutile, and apatite. Suitable for igneous, metamorphic, and detrital studies. Complete service from rock to report (includes processing, imaging and data reduction).
High-precision dating of uranium-bearing minerals including zircon, monazite, baddeleyite, titanite, rutile, and apatite. Suitable for igneous, metamorphic, and detrital studies. Complete service from rock to report (includes processing, imaging and data reduction).
Age determination using Lu-rich minerals such as garnet and apatite. Ideal for dating high-grade metamorphic events, mafic rocks, and reconstructing pressure–temperature paths. Complete service from rock to report (includes processing, imaging and data reduction).
Age determination using Lu-rich minerals such as garnet and apatite. Ideal for dating high-grade metamorphic events, mafic rocks, and reconstructing pressure–temperature paths. Complete service from rock to report (includes processing, imaging and data reduction).
In situ isotopic dating of minerals like biotite, muscovite, and K-feldspar. Useful for low-temperature systems and hydrothermal or deformation histories. Complete service from rock to report (includes processing, imaging and data reduction).
In situ isotopic dating of minerals like biotite, muscovite, and K-feldspar. Useful for low-temperature systems and hydrothermal or deformation histories. Complete service from rock to report (includes processing, imaging and data reduction).
High-precision ⁴⁰Ar/³⁹Ar dating of potassium-bearing minerals such as feldspar, mica, and amphibole. Ideal for constraining thermal histories, volcanic events, and low- to medium-grade metamorphism. Complete service from rock to report (includes imaging and data reduction).
High-precision ⁴⁰Ar/³⁹Ar dating of potassium-bearing minerals such as feldspar, mica, and amphibole. Ideal for constraining thermal histories, volcanic events, and low- to medium-grade metamorphism. Complete service from rock to report (includes imaging and data reduction).
Isotope ratio analysis in zircon and baddeleyite for crustal evolution, mantle input, and source tracing studies. Complete service from rock to report (includes processing, imaging and data reduction).
Isotope ratio analysis in zircon and baddeleyite for crustal evolution, mantle input, and source tracing studies. Complete service from rock to report (includes processing, imaging and data reduction).
Lead isotopic analyses of K-feldspar, sulphides, and whole rocks to track ore-forming processes and crustal evolution. Complete service from rock to report (includes processing, imaging and data reduction).
Lead isotopic analyses of K-feldspar, sulphides, and whole rocks to track ore-forming processes and crustal evolution. Complete service from rock to report (includes processing, imaging and data reduction).
Size (0.01 microns - gravel), shape, and compositional characterisation of mineral and lithic grains. Useful for provenance studies, sediment transport analysis, environmental analysis and detrital mineralogy. Complete service from rock to report (includes processing, imaging and data reduction).
Size (0.01 microns - gravel), shape, and compositional characterisation of mineral and lithic grains. Useful for provenance studies, sediment transport analysis, environmental analysis and detrital mineralogy. Complete service from rock to report (includes processing, imaging and data reduction).
Research groups
CFIGS houses dedicated research groups focused on geoscientific innovation, including Geochronology, Isotope Geology, Petrology, Geodynamics, Earth Materials Characterisation, Resource Systems Analysis, and Environmental Geosciences. Each group brings world-class expertise, diverse perspectives, and cutting-edge methodologies, working collaboratively to transform scientific insight into solutions.
If you’re unsure where to start, simply contact us. Share your challenge, and we’ll connect you with the right experts at CFIGS to explore options, discuss potential collaborations, and shape the pathway to impactful results.
Advances in our understanding of isotopic tracers, isotopic systems, trace element geochemistry, pathfinder elements - these are examples of areas of research that are being used.
Geoscientific spatial datasets allow for informed decisions to be made about all types of land use from agriculture, hydrology through to infrastructure and mining.
One of the main upcoming challenges is to successfully implement AI systems at scale to help geoscientists integrate and interrogate big data in meaningful and grounded ways.
Through breakthroughs in isotopic tracer development, geochemical fingerprinting, and pathfinder element analysis, Curtin University continues to be a World leader in decoding Earth’s hidden geochemical signatures driving both scientific insight and exploration discovery.
Findings delivered by Curtin University continue to unlock discoveries and are therefore a critical component to modern exploration geoscience.
In the event your question isn’t covered in our FAQs, please get in touch using the form on our contact page, or directly using the provided contact details.
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