内蒙古东升庙矿床岩浆热液叠加成矿作用——来自地质与矿物包裹体测温的证据

彭润民 翟裕生 韩雪峰 王建平 王志刚 秦俊文. 内蒙古东升庙矿床岩浆热液叠加成矿作用——来自地质与矿物包裹体测温的证据[J]. 岩石学报, 2007, 23(1): 145-152.
引用本文: 彭润民 翟裕生 韩雪峰 王建平 王志刚 秦俊文. 内蒙古东升庙矿床岩浆热液叠加成矿作用——来自地质与矿物包裹体测温的证据[J]. 岩石学报, 2007, 23(1): 145-152.
PENG RunMin, ZHAI YuSheng, HAN XueFeng, WANG JianPing, WANG ZhiGang,QIN JunWeng. Magmatic hydrothermal overprinting in the Mesoproterozoic Dongshengmiao deposit, Inner Mongolia: geological and fluid inclusion evidences[J]. Acta Petrologica Sinica, 2007, 23(1): 145-152.
Citation: PENG RunMin, ZHAI YuSheng, HAN XueFeng, WANG JianPing, WANG ZhiGang,QIN JunWeng. Magmatic hydrothermal overprinting in the Mesoproterozoic Dongshengmiao deposit, Inner Mongolia: geological and fluid inclusion evidences[J]. Acta Petrologica Sinica, 2007, 23(1): 145-152.

内蒙古东升庙矿床岩浆热液叠加成矿作用——来自地质与矿物包裹体测温的证据

  • 基金项目:

    This research was supported by National Natural Sciences Foundation of China ( Grant No. 40234051 and Grant No. 40572064 ), National Basic Research Program of China (Grant No. 2006CB403503) and Research Program of Inner Mongolia (Grant No. 2004-1-2).

Magmatic hydrothermal overprinting in the Mesoproterozoic Dongshengmiao deposit, Inner Mongolia: geological and fluid inclusion evidences

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出版历程
修回日期:  2006-07-15
刊出日期:  2007-01-31

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