EGU26-5827, updated on 13 Mar 2026
https://doi.org/10.5194/egusphere-egu26-5827
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Friday, 08 May, 08:30–10:15 (CEST), Display time Friday, 08 May, 08:30–12:30
 
Hall X2, X2.97
Helium-based thermochronometry and cosmogenic noble gas geochemistry in the Thermochronology @ Purdue (T@P) noble gas mass spectrometry facility
Marissa M. Tremblay1, Hongcheng Guo1, Eric T. Dziekonski1,2, Ryan B. Ickert1, and Devin Blair1
Marissa M. Tremblay et al.
  • 1Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, United States of America (tremblam@purdue.edu)
  • 2Department of Chemistry, Purdue University, West Lafayette, United States of America

The Thermochronology @ Purdue (T@P) noble gas mass spectrometry facility was established at Purdue University between 2020 and 2023. In this presentation, we will detail the T@P laboratory’s instrument configuration and demonstrate the facility’s capabilities for both helium-based thermochronometry and cosmogenic noble gas geochemistry. The primary instrument in the T@P laboratory is an Isotopx NGX, a multi-collector sector field mass spectrometer with a Nier-type source, which has a custom detector configuration consisting of three discrete dynode electron multipliers, including one fitted with an electrostatic filter, and two Faraday cups with ATONA® amplifiers. The NGX is connected to a custom-built, fully automated, ultra-high vacuum extraction line that includes an activated charcoal cryogenic trap and two getters for gas purification, two manometrically-calibrated gas standards for sensitivity calibration (air and 3He-enriched helium), and a manometrically-calibrated 3He spike for measurements of radiogenic 4He by isotope dilution. Gases are extracted by heating samples under vacuum using a diode laser system in a feedback control loop with either a calibrated optical pyrometer (better than ± 10 ºC precision), or a bare, thin-wire thermocouple in contact with the sample (better than ± 3 ºC precision). We will present isotopic analyses made in the T@P laboratory of reference materials for both helium-based thermochronometry (Durango apatite) and cosmogenic noble gas geochemistry (CRONUS-P, CRONUS-A, CREU-1) as well as from example applications in Earth and planetary surface processes.

How to cite: Tremblay, M. M., Guo, H., Dziekonski, E. T., Ickert, R. B., and Blair, D.: Helium-based thermochronometry and cosmogenic noble gas geochemistry in the Thermochronology @ Purdue (T@P) noble gas mass spectrometry facility, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-5827, https://doi.org/10.5194/egusphere-egu26-5827, 2026.