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《Acta Geoscientica Sinica》 2013-01
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Progress of SinoProbe-Deep Exploration in China 2008—2012

DONG Shu-wen 1),LI Ting-dong 1),GAO Rui 2),Lü Qing-tian 3),WEI Wen-bo 4),YANG Jing-sui 2),WANG Xue-qiu 5),CHEN Qun-ce 6),SHI Yao-lin 7),HUANG Da-nian 8),CHEN Xuan-hua 1),ZHOU Qi 1) 1) Chinese Academy of Geological Sciences,Beijijng 100037;2) Institute of Geology,Chinese Academy of Geological Sciences,Beijijng 100037;3) Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijijng 100037;4) China University of Geosciences(Beijing),Beijing 100083;5) Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang,Hebei 065000;6) Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijijng 100081;7) Graduate University,Chinese Academy of Sciences,Beijing 100049;8) Jilin University,Changchun,Jilin 130026  
The SinoProbe-Deep Exploration in China is a multidisciplinary earth science research program on geosciences with unprecedented scope and scientific ambition.The overall aim of the SinoProbe is to reveal the composition,structure and evolution of the continental lithosphere underneath China.SinoProbe 2008—2012,the initial phase of the SinoProbe,has achieved a lot of technological innovations and made some important scientific discoveries in the field of deep exploration in China,with a great innovation value for the society.The project has completed a total length of 6000 km deep seismic reflection profiling in Tibet,South China,North China,and Northeast China,impelling China to be one of the major advanced countries in the international society of deep exploration.It has carried out lots of research work,such as nation-wide geochemical baseline(with 78 elements) and magnetotelluric(MT) array(by 4°·4°,and 1°·1° in North China and Tibet),3D exploration in ore deposit districts in eastern China,several fruitful continental scientific drilling boreholes,two regional in-situ stress monitoring networks,geodynamic modeling of the lithosphere underneath China's mainland,and instrumentation development for deep exploration in China.As a result,some new recognitions on the Mesozoic-Cenozoic geological and tectonic evolution of the continental China have been gained.In addition,some valuable explorations on the organization and administration of big-science program were made,which have exerted a strong influence on the geoscience society of the world.The SinoProbe 2008—2012 has laid a solid foundation for the organization and implementation of the full scale SinoProbe-Deep Exploration in China as a Major National Science and Technology Program.The SinoProbe is considered as a major signature geoscience program during the transition of China from a big country of geoscience to a powerful country of geoscience.SinoProbe-Deep Exploration in China,opening a new time of geoscience research in China,was awarded one of the top 10 scientific and technological progresses of China in 2011 by the Chinese Academy of Sciences and the Chinese Academy of Engineering,and the international synchronization of the SinoProbe-Deep Exploration in China,has been awarded the Special Progress of the Chinese Academy of Geological Sciences in 2012.
【Fund】: 国家专项“深部探测技术与实验研究”(编号:SinoProbe-08)资助
【CateGory Index】: P313
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