目录
- The copper polymetallic deposits and resource potential in the Tibet Plateau
- Natural gas hydrates in the Qinghai-Tibet Plateau: Characteristics, formation, and evolution
- How does the elevation changing response to crustal thickening process in the central Tibetan Plateau since 120 Ma?
- Behavior of apatite in granitic melts derived from partial melting of muscovite in metasedimentary sources
- Early Eocene leucocratic sill/dike swarms in the Gangdese belt, southern Tibet:Tectonic implications for Indo-Asian collision
- Early Cretaceous deformation in the southern Tashkorgan region: Implications for the tectonic evolution of the northeastern Pamir
- A new understanding of Demala Group complex in Chayu Area, southeastern Qinghai-Tibet Plateau: Evidence from zircon U-Pb and mica 40Ar/39Ar dating
- High pressure garnet amphibolites in ophiolitic mélange from the Changning-Menglian suture zone, southeast Tibetan Plateau: P-T-t path and tectonic implication
- Petrology and metamorphism of glaucophane eclogites in Changning-Menglian suture zone, Bangbing area, southeast Tibetan Plateau: An evidence for Paleo-Tethyan subduction
- Geophysical prospecting of copper-nickel deposits in Beishan rift zone, Xinjiang
- Research achievements of the Qinghai-Tibet Plateau based on 60 years of aeromagnetic surveys
- Microplastic pollution in surface water and sediments of Qinghai-Tibet Plateau: Current status and causes
- The Oligocene tin mineralization in the SE Sanjiang metallogenic belt, SW China
- Successful completion of the first 3000 m scientific deep drilling for solid mineral exploration area on the Qinghai-Tibet Plateau
- China raised the first batch production quota over rare-earths and tungsten in 2021
- Zircon U-Pb age of pegmatite veins in Dahongliutan lithium deposit, western Kunlun