351. A comparative study of ore-forming environments and conditions in Feng-Tai and Zha-Shan orefields, Qinling Mountains.
- Author
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Li Yanhe, Jiang Shaoyong, Xue Chunji., Li Yanhe, Jiang Shaoyong, and Xue Chunji.
- Abstract
A study is presented of Si, O and S stable isotope compositions and variation in the Devonian stratiform Pb-Zn deposits. Delta-30 Si and delta-18 O values for ore-bearing siliceous rocks in the Fengtai orefield indicate a submarine exhalative origin, while those of quartz veins are similar and suggest that the ore veins formed by remobilisation and recrystallisation of the siliceous rocks. The values for the Zhashan orefield apparently indicate a similar submarine exhalative origin but with higher temperature and speed of deposition. Sulphur was exclusively derived from sulphates in sea water, with the Zhashan basin changing from an enclosed basin during the main ore-forming stage to an open one at the late stage while delta-34 S isotope values for Fengtai deposits imply a semi-open to semi-enclosed basin., A study is presented of Si, O and S stable isotope compositions and variation in the Devonian stratiform Pb-Zn deposits. Delta-30 Si and delta-18 O values for ore-bearing siliceous rocks in the Fengtai orefield indicate a submarine exhalative origin, while those of quartz veins are similar and suggest that the ore veins formed by remobilisation and recrystallisation of the siliceous rocks. The values for the Zhashan orefield apparently indicate a similar submarine exhalative origin but with higher temperature and speed of deposition. Sulphur was exclusively derived from sulphates in sea water, with the Zhashan basin changing from an enclosed basin during the main ore-forming stage to an open one at the late stage while delta-34 S isotope values for Fengtai deposits imply a semi-open to semi-enclosed basin.