刘阳.太行山北段麻棚岩体锆石SHRIMP U-Pb年龄及其意义[J].地质与勘探,2010,46(4):622-627 |
太行山北段麻棚岩体锆石SHRIMP U-Pb年龄及其意义 |
The Zircon SHRIMP U-Pb Age of Mapeng Granite Complex in the NorthernTaihang Shan Mountains and Its Implications |
投稿时间:2010-05-19 修订日期:2010-07-05 |
DOI: |
中文关键词: 麻棚岩体 太行山 SHRIMP U-Pb 年龄 |
英文关键词: Mapeng granite complex,Taihang Shan Mountains,SHRIMP,U-Pb age |
基金项目:国家自然科学基金项目(40672150)资助 |
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中文摘要: |
[摘要]在太行山构造-岩浆-多金属成矿带上沿NNE 向发育大量的中-酸性侵入岩,其中太行山
北段阜平南部的麻棚岩体与石湖金矿成矿因素关系紧密,因此倍受关注。本文报道了麻棚岩体北部过
渡带中花岗闪长岩SHRIMP U-Pb 年代学数据(125. 0依3. 4Ma),该年龄是目前已知太行山北段中生代侵
入岩年龄值中最年轻的。同时这一结果表明,直至125Ma,太行山北段的岩浆活动依旧活跃;其次,该年
龄对太行山北段NW 向断裂系统的活动时间进行了限定。 |
英文摘要: |
Abstract:A lot of intermediate acid intrusions are distributed along the tectonic-magmatic-polymetallic metallogenic belt in the Taihang Shan
Mountains of the NEE direction. The Mapeng complex granite in the southern Fuping in the northern Taihang Mountains receives much attention because
of its close relationship with ore-forming elements of the Shihu gold deposit. This paper reports the data of the SHRIMP U-Pb age (125. 0依3. 4 Ma) in
the transitional zone of the northern Mapeng granite complex. This is the youngest among the data of the known Mesozoic intrusions in the northern Taihang
Shan Mountains. Meanwhile,this result shows that until 125 Ma the magmatic activity of the northern Taihang Shan Mountain was still ongoing,and it also
defines the time span of activity of the NW fault-system in this area |
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