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《GEOCHIMICA》 1997-01
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Xue Chunji (Xian College of Geology,Xian 710054)Jiang Shaoyong (Geology Department,University of Bristol,England)Li Yanhe (Institute of Mineral Deposits,Chinese Academy of Geological Sciences,Beijing 100037)  
Tourmaline occurs in an important quantity in the ore bearing bed of most stratabound base metal sulphide ore deposits at Shanyang-Zhashui Devonian metallogenic area in eastern Qin Ling.They belong to the solid solution series of schorl-dravite in which MgFe and NaCa (cation basis).Most of the tourmalines are zoned chemically and the zones recorded the seafloor (exhalative) hydrothermal sedimentary and diagenesis process during the main metallogenic epoch and the subsequent regional metamorphism and hydrothermal overprinting process.The chemical compositions[FeO/(FeO+MgO)=0.34—0.39]and the boron isotopic compositions (δ 11 B=-7.6‰? ?.8‰ ) of the tourmalines formed in the main metallogenic epoch are simelar to those of tourmalines in the seafloor (exhalative) hydrothermal sedimentary massive sulphide ore deposits.This suggests that the seafloor (exhalative) hydrothermal sedimentary process is the main metallogenic mechanism for the stratabound ore deposits in the metallogenic area.
【Fund】: 国家自然科学基金青年基金
【CateGory Index】: P578.953
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