Partial melting caused by subduction of young, hot oceanic crust in shallow high-temperature and low-pressure environments: Indications from Middle and Late Jurassic oceanic plagiogranite in Shiquanhe, Central Tibet
Autor: | Hang, Li, Ming, Wang, Xiao-Wen, Zeng, An-Bo, Luo, Bo-Chuan, Zhang, Di, Shen |
---|---|
Zdroj: | In LITHOS July 2022 420-421 |
Databáze: | ScienceDirect |
Externí odkaz: |