Origin of oscillatory zoned garnets from the Xieertala Fe–Zn skarn deposit, northern China: In situ LA–ICP-MS evidence
2014/01/03 by De-Gao Zhai, Degao Zhai, Jiajun Liu +10 · 149 citations
Earth and Planetary Sciences · #Fluid inclusions #Geochemistry #Geochemistry and Elemental Analysis #Geological and Geochemical Analysis #Geology #Geology and Paleoclimatology Research #Hydrothermal circulation #Mineralogy #Paleontology #Petrography #Rare earth #Rare-earth element #Skarn #Trace element
paper · doi:10.1016/j.lithos.2013.12.017
published in Lithos 190-191, 279-291 (Elsevier BV)
openalex publication_date 2014/01/03 · openalex created_date 2025/10/10 · openalex updated_date 2026/08/04
Citations
Cited by
- The formation and trace elements of garnet in the skarn zone from the Xinqiao Cu-S-Fe-Au deposit, Tongling ore district, Anhui Province, Eastern China
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- Textural and geochemical characteristics of garnet from the Luoyang Fe skarn deposit, eastern China: implications for ore-forming fluid evolution and mineralization conditions
- Origin and Evolution of Oscillatory Zoned Garnet From Kasva Skarn, Northeast Tafresh, Iran
- Genesis of the Baitoushan Cu-Polymetallic Deposit, Qimantagh Region, Eastern Kunlun Orogen: Evidence from geochemistry of garnets and geochronology