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内蒙古韧性剪切带型金矿──十八顷毫矿区40Ar/39Ar坪年龄特征及其地质意义
40Ar/39Ar PLATEAU AGE SPECTRA OF THE SHIBAQINGHAO GOLD DEPOSIT IN THE DUCTILE SREAR ZONE OF INNER MONGOLIA AND THEIR GEOLOGICAL IMPLICATIONS
【摘要】 对采自十八顷毫金矿区的黑云母、角闪石用阶段升温法进行40Ar/39Ar年龄谱研究,结合矿区地质特征,认为黑云母近似直线年龄谱的坪年龄(277Ma)及角闪石稳定坪年龄(288Ma)代表了韧性剪切带最新活动的时代;角闪石矿物年龄谱反映的后期热扰动(268Ma)反映区域退化变质作用发生的时代,269~277Ma的年龄可能代表了与退化变质同时的金矿化时代。
【Abstract】 The Shibaqinghao gold deposit is a typical one occurring in a ductile shear zone in centralInner Mongolia. To gain a better understanding of the age of gold mineralization and its relationship with the evolution of the ductile shear zone,40Ar/39Ar plateau age analysis was made on biotitefrom biotite-quartz gneiss and on hornblende from biotite-hornblende mylonite. The 40Ar/39Arplateau age spectra of biotite are represented by nearly a straight line. The age of 277. 23 Ma standsfor the age of gold mineralization and the latest retrograde metamorphism. The 40Ar/39Ar age spectra of hornblende are normal. The age of 268. 62 Ma means the latest activity of the ductile shearzone, and the age of 268. 5~277. 23 Ma may represent the age of gold mineralization contemperaneous with the retrograde metamorphism.
【Key words】 biotite; hornblende; 40Ar/39Ar plateau age spectra; ductile shear zone;
- 【文献出处】 矿物学报 ,Acta Mineralogica Sinica , 编辑部邮箱 ,1996年01期
- 【分类号】P618.51
- 【被引频次】7
- 【下载频次】121