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REMELTED MAGNETITE GRANITES AND THE ASSOCIATED GOLD DEPOSITS IN THE NORTHWEST PART OF THE JIAODONG PENINSULA

Liu Liandeng Yao Fengliang  
The northwest part of the Jiaodong Peninsula is one of the most important gold metallogenic provinces in China. The congenetic intrusion of the gold deposits is Luanjiahe granite, which is moderate-deep one (Fig. 1) .The granite is believed to be magnetite series, corresponding to I-type granite based on the following characteristics: high content of magnetite and similar accessory mineral assemblage, biotite with high content of iron and low magnesiam (Fig.5), I-type composition of main oxides(Fig.6)and isotopes of Sr,O,S.The evolution of K,Rb,Sr, correlation of the main oxides, inheritance of rare earth elements,and sulphur isotopes also prove that the Luanjiahe granite is magnetite one of lower crust origin, which source rocks corresponds to Jiaodorg Group metamorphic rocks of a U-Pb isochronous age of 2.6 Ga.The main magmatic hydrothcrmal gold lodes are usually located in old metamorphic rocks (mainly in Archean), while the age of mineralization is much younger (mainly in Mesozoic) .They are spacially controlled by structural-magmatic belts. The frequent intrusion of dykes occurred during the mineralization process. These characteristics can be interpreted by the hypothesis proposed here that gold deposits are congenetic with remelted magnetite-series granite of lower-crust origin.
【Fund】: 科学基金
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