Crust-mantle interaction during continental deep subduction: evidence from light Mo isotopes in post-collisional mafic igneous rocks from the East Kunlun orogen

Name: Crust-mantle interaction during continental deep subduction: evidence from light Mo isotopes in post-collisional mafic igneous rocks from the East Kunlun orogen
Published: 2025-04-14T15:10:06+08:00