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《Geology in China》 2012-01
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The discovery of the Lower Cambrian and Middle Ordovician Radiolaria in the South China orogenic belt

ZHENG Ning1,SONG Tian-rui1,LI Ting-dong1,LIU Xun1,GENG Shu-fang1,DING Xiao-zhong1,TAN Zheng-xiu2,YOU Guo-qing1,LING Yue-sheng2 (1.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China;2.Hunan Institute of Geological Survey,Changsha 410000,Hunan,China)  
Radiolaria fossils were discovered for the first time in the lower Cambrian and middle Ordovician strata of the South China orogenic belt.They occur in argillaceous slate of the lower Cambrian Niujiaohe Formation in Pingxiang of Jiangxi Province and silicalite of the middle Ordovician Yanxi Formation in Yongzhou of Hunan Province.The discovery of Radiolaria shows that there might have existed a low-latitude sea basin of considerable scale in Pingxiang-Yongzhou area in Cambrian-Ordovician period.
【Fund】: 中国地质调查局“西太平洋大陆边缘深部过程与成矿作用”项目(1212010733802);“中国地层构造区划与区域地质调查综合集成”项目(1212011120115);“中国构造区划及其在全国地质志中的应用”项目(1212011120117)共同资助
【CateGory Index】: Q915
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