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《MINERAL DEPOSITS》 1994-01
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SULFUR ISOTOOE STUDIES OF THE METALLOGENIC SERIES OF GOLD DEPOSITS IN JIAODONG (EASTERN SHANDONG)AREA

HuangDeye(No. 6 Geological Party,Shandong Bureau of Geology and Mineral Resources,Zhaoyuan County,Shandong Province)  
The endogenic gold deposits in Jiaodong area might be assigned tO twometallogenic epochs:principal(late Jurassic) epoch and accompanying(EarlyCretaceous)epoch,resulting both from the differentiation and evolution of a- natectic magma,In each epoch of the metallongenic serries,δ ̄(34)S values tend to decrease gradually from e arly to late,while things are quite the opposite for δ ̄(18)O values,The anatectic magma formed in the principal mineralization epoch occurred in larger depth,and its δ ̄(34)S values are somewhat high,varying from 8.9‰of the granite through 6.9‰ of the intermediate-basic dikes to 6.7‰ of the gold deposits,In contrast,the anatectic magma formed in the accompanying mineralization epoch occurred in shallower place,and the process of its forma- tion was characterized by the participation of meteoric water and exogenic ore substances;as a result,its δ ̄(34)S values are slightly lower,varying from6.6‰ ofthe early granodiorite through 2.4‰ of the intermediate-basic dikes to-2.6‰ of the ore deposits,These data demonstrate that sulfur isotope fraction mainly follows the principle of thermodynamic effect,whereas oxygen isotope fractio- nation is chiefly restricted by the theorem of kinetic energy.All this has pro- vided the important basis for the establishment of the metallogenic theory of differentiation and evolution of anatectic magma and the metallogenic series. The Jiaojia type gold deposits occur in large-size and gently-dipping tecto-nic shatter zones where large quantities of meteoric water and exogenic ore substances are stored.Once connceting with ore magma,the meteoric water and exogenic ore substanca would particicipate in the ore-forming process,After theore magma was trapped under great confining pressure, exogenic sulfur would be mixed and exchanged with magma sulfur in a reducing environment.The equilibrium temperature between galena and sphalerite would remain stable at the end of the principal ore-forming stage. Hence the δ ̄(34)S values of the Jiaojia type deposits obviously deviate toward the positive side. The participation of exogenic sulfur to the ore-forming process has confused the regularity of sulfur isotope evolution.
【CateGory Index】: P618.510.1
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7 HuangDeye(No. 6 Geological Party,Shandong Bureau of Geology and Mineral Resources,Zhaoyuan County,Shandong Province);SULFUR ISOTOOE STUDIES OF THE METALLOGENIC SERIES OF GOLD DEPOSITS IN JIAODONG (EASTERN SHANDONG)AREA[J];矿床地质;1994-01
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