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云南兰坪白秧坪铜钴多金属矿集区矿石中石英的40Ar-39Ar年龄
引用本文:何明勤,刘家军,李朝阳,李志明,刘玉平,杨爱平,桑海清.云南兰坪白秧坪铜钴多金属矿集区矿石中石英的40Ar-39Ar年龄[J].地质科学,2006,41(4):688-693.
作者姓名:何明勤  刘家军  李朝阳  李志明  刘玉平  杨爱平  桑海清
作者单位:1. 中国科学院地球化学研究所矿床地球化学重点研究实验室, 贵阳, 550002;2. 中国地质大学, 北京, 100083;3. 云南省地质矿产局第三地质大队, 云南, 大理, 671000;4. 中国科学院地质与地球物理研究所, 北京, 100029
基金项目:国家重点基础研究发展计划(973计划),云南省教育厅资助项目
摘    要:云南兰坪白秧坪铜钴多金属矿集区矿石中石英的40Ar-39Ar快中子活化年龄谱呈马鞍形,坪年龄为56.53±0.43Ma,最小视年龄为55.52±1.78Ma,等时线年龄为55.90±0.29Ma,三者在误差范围内一致(1σ)。40Ar/36Ar初始值为294.7±1.14,与尼尔值(295.5±5)十分接近,坪年龄和等时线年龄均可作为石英的形成时代。因此,55.90~56.53Ma(喜马拉雅早期)代表了矿床的成矿年龄。

关 键 词:40Ar-39Ar年龄  喜马拉雅早期  铜钴多金属矿集区  滇西兰坪
文章编号:0563-5020(2006)04-0688-06
收稿时间:2004-01-08
修稿时间:2004-06-24

40Ar-39Ar DATING OF ORE QUARTZ FROM THE BAIYANGPING Cu-Co POLYMETALLIC MINERALIZED CONCENTRATION AREA, LANPING, YUNNAN
He Mingqin,Liu Jiajun,Li Chaoyang,Li Zhiming,Liu Yuping,Yang Aiping,Sang Haiqing.40Ar-39Ar DATING OF ORE QUARTZ FROM THE BAIYANGPING Cu-Co POLYMETALLIC MINERALIZED CONCENTRATION AREA, LANPING, YUNNAN[J].Chinese Journal of Geology,2006,41(4):688-693.
Authors:He Mingqin  Liu Jiajun  Li Chaoyang  Li Zhiming  Liu Yuping  Yang Aiping  Sang Haiqing
Institution:1. Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002;2. China University of Geosciences, Beijing 100083;3. No.3 Geological Party, Bureau of Geology and Mineral Resources of Yunnan Province, Dali, Yunnan 671000;4. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029
Abstract:40Ar-39Ar fast neutron activation age spectrum of quartz in ore collected from the Baiyangping Cu-Co polymetallic mineralized concentration area in Lanping,Yunnan, showed a characteristic of saddle shape. The obtained plateau age,minimum appearance age and isochron age of the spectra were 56.53±0.43 Ma,55.52±1.78 Ma and 55.90±0.29 Ma respectively, all of three ages being identical within 1σ uncertainties. Both of the plateau and isochron ages could be regarded as the quartz’s forming time, since the given 40Ar/36Ar initial value of 294.7±1.14 was very close to Nier’s value (295.5±5), namely, the age of 55.90~56.53 Ma (Early Himalayan period) represented the ore deposits’forming age.
Keywords:^40Ar-^39Ar dating  Early Himalaya  Cu-Co polymetallic mineralized concentration area  Lanping in western Yunnan
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