Speaker: Ian Campbell (RSES, ANU)
The changes that occur at the boundary between the Archean and Proterozoic eons are arguably the most fundamental to affect the evolution of Earth’s continental crust.
Performance of the Helix MC Plus noble gas mass spectrometer installed at the Australian National University (ANU) is reported.
Speaker: Zsanett Pintér (Macquarie University, BGI Germany)
Many mantle-derived magmas may originate through partial melting of complex, mixed mantle rocks including not only peridotite, but also oceanic crust recycled into the mantle.