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地球科学进展  2008, Vol. 23 Issue (4): 421-427    DOI: 10.11867/j.issn.1001-8166.2008.04.0421
“土地利用/覆盖变化与综合减灾”专辑     
矿床变化与保存研究的裂变径迹新途径
王建平,翟裕生,刘家军,柳振江,刘 俊
中国地质大学(北京)地质过程与矿产资源国家重点实验室,岩石圈构造、深部过程及探测技术教育部重点实验室,北京 100083
A New Approach to Post-ore Change and Preservation of Ore Deposits: Fission Track Analysis
Wang Jianping,Zhai Yusheng,LiuJiajun,Liu Zhenjiang,Liu Jun
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Key Laboratory of Lithospheric Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China
 全文: PDF(1158 KB)  
摘要:

矿床形成后的变化与保存是矿床学研究与找矿勘探中一项极其重要但仍需进一步加强的基础性工作。影响矿床变化与保存的众多因素中,区域隆升与剥蚀是最为关键的因素之一。裂变径迹法是研究区域隆升与剥蚀的一种有效手段,它能为我们提供剥蚀速率以及剥蚀量的定量数据。一些产于花岗质岩体内与岩体有成因联系的矿床,其成矿深度可以通过详细的流体包裹体研究来获得。通过成矿深度与岩体剥蚀深度对比分析,能使我们更好地了解矿床形成后变化保存条件。裂变径迹法与流体包裹体研究相结合是矿床形成后变化与保存研究一种切实可行的方法

关键词: 成矿系统成矿后变化与保存裂变径迹成矿深度剥蚀深    
Abstract:

Post-ore change and preservation, an aspect should be pay more attention, is a basic problem both to ore deposit geology and to mineral exploration. Regional uplift and denudation is the most important factors affecting post-ore change and preservation of ore deposits. While fission track method is an effective way to study regional uplift and denudation, it can provide us denudation rate and degree quantitatively. Taking some ore deposits closely related to granitic intrusions as examples, ore-forming depth can be calculated through fluid inclusion study. Thus comparison between ore-forming depth and post-ore denudation will led better understand of post-ore change and preservation of ore deposits. Fission track method combining with fluid inclusion study will be a practical approach to post-ore change and preservation in the study of ore deposit geology.

Key words: Metallogenic system    Post-ore change and preservation    Fission track method    Ore-forming depth    Denudation depth.  
收稿日期: 2007-11-05 出版日期: 2004-04-10
:  P611  
基金资助:

国家重点基础研究发展计划项目“华北大陆边缘造山过程与成矿”(编号:2006CB403503) ;国家自然科学基金面上项目“胶东玲珑花岗质杂岩的隆升剥蚀及对其中金矿形成后变化保存的制约”(编号:40602010);中国地质大学地质过程与矿产资源国家重点实验室开放基金项目“焦家金矿田形成后变化保存研究——玲珑杂岩体剥蚀程度的制约”(编号:GPMR0737)联合资助.

通讯作者: 王建平     E-mail: jpwang@cugb.edu.cn
作者简介: 王建平(1972-),男,河北昌黎人,副教授,现主要从事金属矿产资源的教学与科研工作.E-mail:jpwang@cugb.edu.cn
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引用本文:

王建平,翟裕生,刘家军,柳振江,刘 俊. 矿床变化与保存研究的裂变径迹新途径[J]. 地球科学进展, 2008, 23(4): 421-427.

Wang Jianping,Zhai Yusheng,LiuJiajun,Liu Zhenjiang,Liu Jun. A New Approach to Post-ore Change and Preservation of Ore Deposits: Fission Track Analysis. Advances in Earth Science, 2008, 23(4): 421-427.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2008.04.0421        http://www.adearth.ac.cn/CN/Y2008/V23/I4/421

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