利用磷灰石裂变径迹法研究金顶铅锌矿成矿时代 |
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引用本文: | 李小明,谭凯旋,龚文君,龚革联.利用磷灰石裂变径迹法研究金顶铅锌矿成矿时代[J].大地构造与成矿学,2000,24(3):283-286. |
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作者姓名: | 李小明 谭凯旋 龚文君 龚革联 |
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作者单位: | 中国科学院长沙大地构造研究所,湖南,长沙,410013 |
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基金项目: | 国家自然科学基金;49702024; |
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摘 要: | 矿物的裂变径迹年龄分析可有效地用于热液矿床成矿时代的研究。对金顶超大型铅锌矿床的成矿年龄存在不同的看法,本文以架崖山矿段为代表,采用磷灰石裂变径迹分析方法测定了金顶铅锌矿床的成矿年龄。结果表明:金顶铅锌矿床的成矿期在渐新世,其后遭受了喜马拉雅造山运动的热扰动。
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关 键 词: | 裂变径迹 成矿时代 金顶铅锌矿 |
修稿时间: | : |
STUDY ON THE METALLOGENIC EPOCH OF THE JINDING LEAD-ZINC DEPOSIT WITH APATITE FISSION TRACK ANALYSIS |
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Abstract: | : Fission track analysis of minerals may be effective in the study of the metallogenic epoch of hydrothermal deposits.There exist different views on the metallogenic age of the Jinding super- large lead- zinc deposit.Taking the Jiayashan ore block as an example,the paper studied the metallogenic epoch of the Jinding lead- zinc deposit with apatite fission track analysis.The result shows that the metallogenic age of the Jinding lead- zinc deposit is the Eocene,and later,the deposit had undergone thermal disturbance of the Himalaya orogenic movement. |
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Keywords: | Fission track metallogenic epoch Jinding lead- zinc deposit |
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