ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
构造动力体制转换与成矿作用
  
关键词:tectonic and dynamic regime  mineralization  tectonic physicochemical parameter  critical transition  induced transition
基金项目:国土资源部地质调查项目(K1.415),国家地质调查局项目(200110200069),中国地质科学院地质调查项目(DKD2101028)联合资助
作者单位
翟裕生 中国地质大学北京100083 
吕古贤 中国地质科学院地质力学研究所北京100081 
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摘要:
Transition of Tectonic and Dynamic Regime and Mineralization
      In the process of mineralization, transition of tectonic and dynamic regime may play a fundamental role, controlling the critical transition and forms of mineralization parameters. Taking gold deposits in Jiaodong as an example, combined with related problems both in China and abroad,this paper illustrates multi-dimension transition of tectonic and dynamic regime and its induced accidental geological process and associated mineralization, describes in detail the critical transition phenomena in the shear-belt structure, and points emphatically out that the local transition under the overall structural setting (e.g. local extension under the overall compressional setting and local trap under the full-apart basin) is a common ore source-transportation-concentration structure. Driven by transition of tectonic and dynamic regime, the induced transition of multi-parameters serves as one of the mechanisms for forming large-size deposits.
ZHAI Yu-sheng,LV Gu-xian.2002.Transition of Tectonic and Dynamic Regime and Mineralization[J].Acta Geoscientica Sinica,23(2):97-102.
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