| 花岗岩类源岩与深部地质作用关系研究的若干进展 |
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| 引用本文： | 邱瑞照,彭松柏.花岗岩类源岩与深部地质作用关系研究的若干进展[J].湖南地质,1998,17(4):276-279. |
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| 作者姓名： | 邱瑞照 彭松柏 |
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| 作者单位： | 中国地质科学院宜昌地质矿产研究所 |
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| 基金项目： | 国家自然科学基金,地质行业科学技术发展基金 |
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| 摘 要： | 花岗岩类源岩研究是成岩成矿物质演化过程研究的基础，各种各样花岗岩的存在归因于花岗岩源岩存在多样性，在不同层圈发生交代，熔融，同化，混染作用；同时，成矿元素亦存在不同深度层圈的多来源，在花岗岩成岩成矿过程中，岩石圈地幔起着重要作用。
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| 关 键 词： | 花岗岩类源岩 深部地质作用 花岗岩 多金属矿床 |
SOME MAKING HEADWAY OF THE RELATIONSHIP BETWEEN GRANITICAL PROTOLYTE AND DEPTH GEOLOGISM |
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| Qiu Ruizhao Peng Songbai Liu GuanliangYichang Institute of Geology and Mineral Resource,CAGS,Yichang.SOME MAKING HEADWAY OF THE RELATIONSHIP BETWEEN GRANITICAL PROTOLYTE AND DEPTH GEOLOGISM[J].Hunan Geology,1998,17(4):276-279. |
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| Authors: | Qiu Ruizhao Peng Songbai Liu GuanliangYichang Institute of Geology and Mineral Resource CAGS Yichang |
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| Institution: | Qiu Ruizhao Peng Songbai Liu GuanliangYichang Institute of Geology and Mineral Resource,CAGS,Yichang,43003 |
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| Abstract: | Granitical protolyte studying is the foundation on the process of material evolution of rock-forming and mineralization.There are varied granitoid,caused by granitical protolyte can be diversity,partial melting can take place in different position of crust-mantle and happen assimilation and hydridism,Mean while,ore-forming elements come from different position of lithosphere,lithosphere-mantle has great function in the process of granitical rock-forming and mineralization. |
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| Keywords: | Headway Granitical protolyte Depth geologism |
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