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《Geotectonica Et Metallogenia》 2003-01
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CHARACTERISTICS OF THE VOLCANIC ROCKS IN DAPINGZHANG,WESTERN YUNNAN AND THEIR TECTONIC SETTINGS

LI Feng, FAN Zhu guo and LI Bao zhu(Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, China)  
The ore bearing formation (Longdonghe Formation), located in the Dapingzhang Cu polymetal deposit in western Yunnan, is mainly composed of spilite, keratophre, quartz keratophyre, rhyolite and siliceous rock with some intermediate acid pyroclastics and tuffites, and belong to the biomodal volcanic association. All rocks exhibit the typical geochemical features of N2OK2O and remarkable depletion of Nb, Ta, Zr, Hf, Ti. Especially, various petrochemical and trace element discrimination signs of the volcanic rocks indicate that the ore bearing formation in the studied area was developed in a special tectonic setting belonging to a rift basin within island arc. Combined with the data analyses of the regional tectonic palaeogeography, it is pointed out that the ore bearing formation is the result of magmatism due to eastward subduction of the palaeo. Tethys oceanic crust in southwestern Yunnan during late Carboniferous to early Permian.
【Fund】: 云南省自然科学基金项目(编号:97D031M;99D0023M).
【CateGory Index】: P588.1
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