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| 构造物理化学成矿理论问题探讨 | |
| 引用本文： | 吕古贤,邓军,倪师军,李晓波.构造物理化学成矿理论问题探讨[J].大地构造与成矿学,2003,27(3):250-263. |
| 作者姓名： | 吕古贤 邓军 倪师军 李晓波 |
| 作者单位： | 1. 中国地质科学院地质力学研究所,北京,100081 2. 中国地质大学(北京),北京,100083 3. 成都理工大学,成都,610059 4. 国土资源部信息中心,北京,100812 |
| 基金项目： | 国土资源部科技发展计划项目(2002201)，中国地质调查局地质调查项目(200110000005)资助. |
| 摘 要： | 构造物理化学成矿研究涉及以下新的认识:构造体制下矿源岩系演化序列,构造动力热液淬取成矿机制,构造附加动力驱动热液成矿机制,构造应力场转化成矿机制,成矿流体水-岩反应的浓缩成矿机制以及构造物理化学场结构与界面成矿特点。 |
| 关 键 词： | 构造物理化学 矿源岩系 构造变形岩相形迹 构造附加静水压力 构造应力场转化 矿化趋势度 构造物理化学界面成矿 |
| 文章编号： | 1001-1552(2003)03-0250-14 |
| 修稿时间： | 2002年10月28日 |
RESEARCH ON METALLOGENETIC THEORY OF TECTONO PHYSICOCHEMISTRY |
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| LU Gu-xian ,DEN Jun ,NI Shi-jun and LI Xiao-bo.RESEARCH ON METALLOGENETIC THEORY OF TECTONO PHYSICOCHEMISTRY[J].Geotectonica et Metallogenia,2003,27(3):250-263. | |
| Authors: | LU Gu-xian DEN Jun NI Shi-jun and LI Xiao-bo |
| Institution: | LU Gu-xian 1,DEN Jun 2,NI Shi-jun 3 and LI Xiao-bo 4 |
| Abstract: | Tectono-physicochemistry is a rese arch field that deals with the interr elations between physical and chemical changes of crustal materia ls caused by tectonism.Tectono-physicochemistry pays special attention to these new researches:crust-mantle superimposing and ore source evolution se ries under a tectonic regime,metall ogenic mechanism of tectonic dynamic leach ing,mechanism of liquid mineraliza tion drived by tectonic driving forc e,metallogenic mechanism of tectonic stress field transformation,water-rock metasomatism and liquid concentrating mineralization and interface mineralization of tectono-physicochemi stry field.This research not only has a great significance for theoretical explo ration but also is of great practical value for predicting hidden mineral deposits,constructing the tectonic evolutio n model for the formation of ultrahig h-pressure metamorphic rocks and studying the driving force of petroleum migratio n.So it is gradually developed into a n independent field of science. |
| Keywords: | Gold deposits Tectono-physicochemistry Ore source evolutions serie s Additional tectonic stress-induced hydrostatic pressure Tectonic stress field transformation L iquid concentrating Mineralization trending degree Interface mineralization o f |
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