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作 者:彭松柏 Timothy M Kusky 周汉文 王璐 项伟
机构地区:[1]Three Gorges Research Center for Geo-hazard,Ministry of Education,China University of Geosciences [2]Faculty of Earth Sciences,China University of Geosciences [3]Three Gorges Research Center for Geo-hazard,Ministry of Education,China University of Geosciences [4]State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences [5]Faculty of Engineering,China University of Geosciences
出 处:《Journal of Earth Science》2012年第5期639-647,共9页地球科学学刊(英文版)
基 金:supported by the Ministry of Land and Resources of China (No. 1212010670104);the National Natural Science Foundation of China (Nos. 91014002, 40821061,41272242);the National Science and Technology Ministry, the Postdoctoral Science Foundation (No. 20100471203);Ministry of Education of China (Nos. B07039, TGRC201024);the Regional Earth Science Background Research for Geological Hazards
摘 要:In this paper the authors briefly introduce and review the new progress of the newly dis-covered Proterozoic Miaowan (庙湾) ophiolite and Neoproterozoic HuangUng (黄陵) granitoids in the southern Huangling anticline in the Yangtze craton, and the tectonic evolution significance of assemblage and breakup of Rodinia and Columbia supereontinent in South China.In this paper the authors briefly introduce and review the new progress of the newly dis-covered Proterozoic Miaowan (庙湾) ophiolite and Neoproterozoic HuangUng (黄陵) granitoids in the southern Huangling anticline in the Yangtze craton, and the tectonic evolution significance of assemblage and breakup of Rodinia and Columbia supereontinent in South China.
关 键 词:Yangtze craton South China HuanglingRodinia andanticline Proterozoic ophiolite Columbia supercontinent.
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