In situ Sr isotopic analyses of epidote: tracing the sources of multi-stage fluids in ultrahigh-pressure eclogite (Ganghe, Dabie terrane)

Shun Guo(Chinese Academy of Sciences), Yuguang Ma(Chinese Academy of Sciences), Kai Ye(Chinese Academy of Sciences), Yue‐Heng Yang(Chinese Academy of Sciences), Qian Mao(Chinese Academy of Sciences), Yi Chen(Institute of Tibetan Plateau Research), Lingmin Zhang(Tongji University), Jingbo Liu(Fujian Medical University)
Contributions to Mineralogy and Petrology
February 1, 2014
10.1007/s00410-014-0975-9
Cited by 33

Related Papers

Contrasting Late Carboniferous and Late Permian-Middle Triassic intrusive suites from the northern margin of the North China craton: Geochronology, petrogenesis, and tectonic implications
|Geological Society of America Bulletin|2006|431
Mineral Inclusions in Zircon from Gneisses in the Ultrahigh‐Pressure Zone of the Dabie Mountains, China
|The Journal of Geology|2001|169
Fluid–rock interaction and element mobilization in UHP metabasalt: Constraints from an omphacite–epidote vein and host eclogites in the Dabie orogen
|Lithos|2011|90
A transitional eclogite- to high pressure granulite-facies overprint on coesite–eclogite at Taohang in the Sulu ultrahigh-pressure terrane, Eastern China
|Lithos|2000|89
Nitrogen-doped carbon encapsulated trimetallic CoNiFe alloy nanoparticles decorated carbon nanotube hybrid composites modified separator for lithium‑sulfur batteries
|Journal of Energy Storage|2024|88