Thermochronology of zircon and apatite to determine cooling and exhumation histories within the 30–300 °C temperature range. Complete service from rock to report (includes processing, imaging and data reduction).
Thermochronology of zircon and apatite to determine cooling and exhumation histories within the 30–300 °C temperature range. Complete service from rock to report (includes processing, imaging and data reduction).
Integrated field mapping, petrography, and geochronology to resolve complex structures and metamorphic histories in granulite-facies terranes. Supports tectonic reconstruction and crustal evolution models.
Integrated field mapping, petrography, and geochronology to resolve complex structures and metamorphic histories in granulite-facies terranes. Supports tectonic reconstruction and crustal evolution models.
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).
Predict the geographical ranges of species based on their relationship with climate.
Predict the geographical ranges of species based on their relationship with climate.
With global temperatures shifting each year, a climatic hazard can trigger cascading effects. As a result, multi-hazard mapping has become a valuable tool for addressing the challenges of a changing climate.
With global temperatures shifting each year, a climatic hazard can trigger cascading effects. As a result, multi-hazard mapping has become a valuable tool for addressing the challenges of a changing climate.
Comprehensive multi-element geochemical analysis across a wide range of minerals for petrogenetic and mineral system interpretation. Complete service from rock to report (includes imaging and data reduction).
Comprehensive multi-element geochemical analysis across a wide range of minerals for petrogenetic and mineral system interpretation. Complete service from rock to report (includes imaging and data reduction).
Thermodynamic modelling of mineral stability and reaction textures using software like THERMOCALC or Perple_X. Used to constrain metamorphic conditions and P–T paths.
Thermodynamic modelling of mineral stability and reaction textures using software like THERMOCALC or Perple_X. Used to constrain metamorphic conditions and P–T paths.
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).
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
C-FIGS 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 C-FIGS to explore options, discuss potential collaborations, and shape the pathway to impactful results.
Just add (mantle) water: new research cracks the mystery of how the first continents formed
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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