Crust-mantle interaction during continental deep subduction: evidence from light Mo isotopes in post-collisional mafic igneous rocks from the East Kunlun orogen
Supplementary material for Brown (2024), PhD thesis - Chapter 8 - High thermal gradient continental subduction initiated by back-arc collapse – evidence from remote south-west TasmaniaExtended methods
Table S1. Major and trace elements and age data summary. Table S2. Zircon U-Pb ages. Table S3. Mineral major elements. Table S4. Zircon trace elements. Table S5. Published ages of the Oligocen
