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下扬子克拉通岩石圈减薄事件与长江中下游Cu-Fe成矿带
LITHOSPHERIC THINNING EVENT IN THE LOWER YANGTZE CRATON AND Cu-Fe METALLOGENIC BELT IN THE MIDDLE AND LOWER YANGTZE RIVER REACHES
【摘要】 在建立下扬子地区中生代地质事件序列的基础上,论证了大别山和下扬子地区印支期和燕山期存在两次相对独立的造山运动,并着重分析了下扬子地区燕山期出现大规模岩石减薄作用的过程,以及与之有关的大规模的成矿作用,并为区内开展深部找矿工作做了某些理论阐述。
【Abstract】 After sorting out Mesozoic geological events in the lower Yangtze area the authors suggested that there existed two relatively independent orogenic movements in the Dabieshan and lower Yangtze areas during the Indosinian and Yenshanian periods, especially the Yenshanian large-scaled lithospheric thinning process in the lower Yangtze area and the relevant mineralization. Comments are also made on deep-seated ore-prospecting work.
【关键词】 地质事件序列,岩石圈减薄;
金属巨量堆积;
长江中下游地区;
【Key words】 order of geological events; lithospheric thinning; huge metallic accumulation; middle and lower Yangtze River reaches;
【Key words】 order of geological events; lithospheric thinning; huge metallic accumulation; middle and lower Yangtze River reaches;
【基金】 中国地调局综合研究项目(K1.4-2-2,K1.4-1-2,200113900018);国土资源部科技专项计划项目(20001010202)的联合资助。
- 【文献出处】 安徽地质 ,Geology of Anhui , 编辑部邮箱 ,2001年02期
- 【分类号】P588.3
- 【被引频次】148
- 【下载频次】655