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长江中下游成矿带及典型矿集区深部结构探测——SinoProbe-03年度进展综述
引用本文:吕庆田,史大年,汤井田,吴明安,常印佛,SinoProbe--CJ项目组.长江中下游成矿带及典型矿集区深部结构探测——SinoProbe-03年度进展综述[J].地球学报,2011,32(3):257-268.
作者姓名:吕庆田  史大年  汤井田  吴明安  常印佛  SinoProbe--CJ项目组
作者单位:中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室;中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室;中南大学地球科学与信息物理学院;安徽省地质调查院;安徽省国土资源厅
基金项目:“深部矿产资源立体探测技术与试验”(编号: SinoProbe-03); 国家自然科学基金重点基金项目(编号: 40930418)
摘    要:大陆现今的地壳结构和物质组成是地壳经历了复杂的动力学演化过程形成的"产品",保留着演化过程中重大地质事件留下的痕迹,使用现代地球物理探测技术对这个"产品"进行成像,不仅可以了解现今的构造和物质状态,还可以推演过去曾经发生的动力学过程.长江中下游成矿带是我国重要的铁、铜多金属资源基地,其形成的深部动力学过程一直是矿床学家...

关 键 词:宽频地震  反射地震  大地电磁  层析成像  各向异性  接收函数  地壳结构

Probing on Deep Structure of Middle and Lower Reaches of the Yangtze Metallogenic Belt and Typical Ore Concentration Area: A Review of Annual Progress of SinoProbe-03
Institution:MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences;MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences;School of Geosciences and Info-physics, Central South University;Geological Survey of Anhui Province;Department of land and Resources of Anhui Provinces
Abstract:The present crustal structure and composition are "products" of complex geodynamic processes through geological time,which maintains the relics and fabrics formed during the major geological movement.The image of the "products" based on modern geophysical technology can help not only comprehend the current state of the structure and material,but also deduce the geodynamic events occurred in the geological time.The middle and lower reaches of Yangtze River metallogenic belt is an important iron,copper and polymetallic base in China,whose deep dynamic processes have constituted the debate focus among researchers.In 2010,a broadband seismic detection about 300km long has been performed in this belt by SinoProbe-03 project,and five seismic reflection,MT and geochemical profiles totally 250km long have been completed over Lujiang-Zongyang ore concentration area.A couple of significant discoveries were made on the basis of preliminary processing and analysis,such as the existence of low-velocity bodies in the upper mantle of the metallogenic belt,short-distance variations of upper mantle anisotropy,local Moho uplift,blur interface between lithosphere and asthenosphere,double-layer crustal structure with thicker upper crust than lower crust.The reflection pattern of crust indicates that it has experienced early compression and later extensional deformation.These discoveries support the dynamic model of asthenosphere uplift,lithospheric thinning,melting of enriched mantle and lower crust thickening and delamination.With these discovers,the extensive development of Cretaceous adakite,shoshonite in metallogenic belt and the causes for the formation of the giant Yangtze River metallogenic belt can also be explained.
Keywords:Broadband Seismics  Reflection Seismics  Magnetotelluric  Tomography  Anisotropy  Receiver  function  Crustal structure
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