地质流体与成矿作用浅析 |
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引用本文: | 杨跃,;张清林,;张俊海,;刘志荣,;王科文.地质流体与成矿作用浅析[J].四川建材,2014(6):226-227. |
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作者姓名: | 杨跃 ;张清林 ;张俊海 ;刘志荣 ;王科文 |
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作者单位: | [1]成都理工大学地球科学学院,四川成都610059; [2]山西省电力勘测设计院,山西太原030001; [3]云南黄金矿业集团股份有限公司,云南昆明650224 |
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摘 要: | 地质流体是在一定地质条件下、通过一定地质作用(包括构造活动、岩浆作用、变质作用、沉积作用、成矿作用、地表作用等)而形成的天然流体。不同特征的地质流体记录了其形成地质环境条件,并代表了特定的地质作用事件和过程。同时,地质流体是地质作用中不可缺少的介质,它几乎参与所有的地质作用,而其中相关的成矿作用是本文关心的内容。
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关 键 词: | 地质流体 热液成矿 成矿作用 |
The Shallows of Geological Fluid and Mineralization |
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Affiliation: | YANG Yue , ZHANG Qinglin , ZHANG Junhai LIU Zhirong, WANG Kewen ( 1. College of Earth Science, Chengdu University of Technology, Chengdu 610059, China; 2. Shanxi Electric Power Exploration & Design Institute, Taiyuan 030001, China; 3. Yunnan Gold Mining Industry Group, Kunming 650224, China) |
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Abstract: | Geological fluid is natural fluid that formed un- der certain geological conditions and processes( including tecton- ic activities, magmatism and metamorphism, sedimentation, mineralization, surface effect, etc. ). Different characteristics of a geological fluid recorded the conditions in which it was formed, and could represent particulars geological effect events and process. At the same time, geological fluid is an indispen- sable medium in geological effecting. It is involved in almost all geological effects, among which the mineralization is the major concern of this thesis. |
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Keywords: | geological fluid hydrotherm mineralization |
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