Unlocking the Potential of Stable Isotopes to Constrain Thermal Histories: Early Steps Toward a Versatile Tool for Diffusion Chronometry Using Chemical-Isotopic Profiles in Zoned Minerals


Corliss Kin I Sio, Lawrence Livermore National Laboratory, Livermore, CA, United States and James Daniel Paul Moore, Earth Observatory of Singapore, Singapore, Singapore
Back to: Origin and Timescales of Magmatic Systems: Discussing Ages, Rates, Transport, and Storage Processes of Magmas from the Source to Emplacement or Eruption II