Area of research
Geophysics · Artificial Intelligence
Research interest
Research interests include Geological and Geochemical Analysis, Geochemistry and Geologic Mapping, Geology and Paleoclimatology Research, and earthquake and tectonic studies.
High-precision U-Pb zircon dating identifies a major magmatic event on the Moon at 4.338 Ga
Recommendations for the reporting and interpretation of isotope dilution U-Pb geochronological information
To sink, or not to sink: The thermal and density structure of the modern northern Andean arc constrained by xenolith petrology
Titanium and iron isotopic records of granitoid crust production in diverse Archean cratons
Zircon U‐Pb Geochronology Constrains Continental Expression of Great Meteor Hotspot Magmatism
Widespread silicic and alkaline magmatism synchronous with the Deccan Traps flood basalts, India
<scp>GZ</scp>7 and <scp>GZ</scp>8 – Two Zircon Reference Materials for <scp>SIMS</scp> U‐Pb Geochronology
<scp>GHR</scp>1 Zircon – A New Eocene Natural Reference Material for Microbeam U‐Pb Geochronology and Hf Isotopic Analysis of Zircon
A New Workflow to Assess Emplacement Duration and Melt Residence Time of Compositionally Diverse Magmas Emplaced in a Sub-volcanic Reservoir
Early formation of the Moon 4.51 billion years ago
Geochronology and Thermochronology
Zircon age-temperature-compositional spectra in plutonic rocks
Temporal variation in relative zircon abundance throughout Earth history
Paleoarchean bedrock lithologies across the Makhonjwa Mountains of South Africa and Swaziland linked to geochemical, magnetic and tectonic data reveal early plate tectonic genes flanking subduction margins
Community‐Derived Standards for <scp>LA</scp>‐<scp>ICP</scp>‐<scp>MS</scp> U‐(Th‐)Pb Geochronology – Uncertainty Propagation, Age Interpretation and Data Reporting
Metrology and traceability of U–Pb isotope dilution geochronology (EARTHTIME Tracer Calibration Part I)
Evaluating uncertainties in the calibration of isotopic reference materials and multi-element isotopic tracers (EARTHTIME Tracer Calibration Part II)
Volcanic–plutonic parity and the differentiation of the continental crust
Evaluating the construction and evolution of upper crustal magma reservoirs with coupled U/Pb zircon geochronology and thermal modeling: A case study from the Mt. Capanne pluton (Elba, Italy)
Stratigraphic expression of Earth's deepest 13C excursion in the Wonoka Formation of South Australia
U-Pb geochronology of the Deccan Traps and relation to the end-Cretaceous mass extinction
Rates of magma differentiation and emplacement in a ballooning pluton recorded by U–Pb TIMS-TEA, Adamello batholith, Italy
Collaborative Research: NSFGEO/NERC: After the cataclysm: cryptic degassing and delayed recovery in the wake of Large Igneous Province volcanism
Collaborative Research: Using K-feldspar megacryst and mineral inclusion T-X-t histories to assess batholith growth and evolution in the Tuolumne intrusive complex, CA
Collaborative Research: Understanding the Tectonic and Petrological Processes Controlling Iron Oxide-Apatite Mineralization in a Mesoproterozoic Collisional Orogen
2021 Gordon Research Conference and Seminar on Geochronology: Evolution of the Lithosphere
Collaborative Research: Testing Models for Early Paleozoic Deposition, Volcanism, and Biotas of Sibumasu: Implications for Tectonics and Paleogeography
Collaborative Research: How are Rhyolites Generated? Evaluating Models for the Volcanic-plutonic Connection in the Searchlight Magmatic System, Nevada
Laboratory Technician Support: Expanding the capacity for U-Pb geochronology at Princeton University
MRI: Acquisition of a Thermal Ionization Mass Spectrometer for High-Precision Geochronology and Isotope Geology
Collaborative research: Andean Plutonic Perspectives on Generation, Storage, and Eruption of Rhyolite
Collaborative Research: Testing the Hypothesis that Bigger Magma Chambers Crystallize Faster
A high-precision U-Pb age model for the Deccan Traps
Collaborative Research: EarthScope Geochronology Graduate Student Training Program
Testing Models for Magma Transfer and Emplacement In 4-Dimensions:The Bergell Intrusion, N. Italy