| SHRIMP Age and Geochemistry of the Bikou Volcanic Terrane: Implications for Neoproterozoic Tectonics on the Northern Margin of the Yangtze Craton |
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| 作者姓名： | A.D.HANSON P.A.DRUSCHKE |
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| 作者单位： | Department of Geosciences，University of Nevada，Las Vegas，Las Vegas，NV 89154-4010，USA，Department of Geosciences，University of Nevada，Las Vegas，Las Vegas，NV 89154-4010，USA |
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| 基金项目： | 国家自然科学基金，科技部资助项目，the China Geological Society of America(to Druschke)are gratefully appreciated |
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| 摘 要： | The Bikou volcanic terrane is predominated by subalkaline tholeiitic lavas. Rock samples display lower initial ratios of Sr and Nd, 0.701248-0.704413 and 0.511080-0.512341 respectively. 207Pb and 208Pb are significantly enriched in the lavas. Most samples have positive εNd, which indicates that the magma was derived from EM-type mantle source, while a few samples with negative εNd indicate that there was contamination in the magma evolution. Magma differentiation is demonstrated by variations of LREE and LILE from depletion to enrichment. Additionally, normalized REE patterns and trace elements showed that lavas from the Bikou volcanic terrane have similar characteristics to those of basalts in arc settings caused by subduction and collision. Analyses showed that the Bikou volcanic terrane is a volcanic arc. New evidence proved that the Hengdan Group, north of the Bikou arc, is a turbidite terrane filling a forearc basin. Consequently, the Bikou volcanic terrane and the Hengdan turbidite terrane const
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| 关 键 词： | 地球化学 火山岩层 克拉通 长江 |
SHRIMP Age and Geochemistry of the Bikou Volcanic Terrane: Implications for Neoproterozoic Tectonics on the Northern Margin of the Yangtze Craton |
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| Authors: | YAN Quanren WANG Zongqi A D HANSON P A DRUSCHKE YAN Zhen LIUDunyi JIAN Ping SONG Biao WANG Tao and JIANG Chunfa Institute of Geology Chinese Academy of Geological Sciences Beijing |
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| Institution: | YAN Quanren,WANG Zongqi,A. D. HANSON,P. A. DRUSCHKE,YAN Zhen,LIUDunyi,JIAN Ping,SONG Biao,WANG Tao and JIANG Chunfa Institute of Geology,Chinese Academy of Geological Sciences,Beijing,Department of Geosciences,University of Nevad,Las Vegas,Las Vegas,NV -,USA Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing |
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| Abstract: | The Bikou volcanic terrane is predominated by subalkaline tholeiitic lavas. Rock samples display lower initialratios of Sr and Nd, 0.701248-0.704413 and 0.511080-0.512341 respectively. 207pb and 208pb are significantly enriched inthe lavas. Most samples have positive εNd, which indicates that the magma was derived from EM-type mantle source,while a few samples with negative εNd indicate that there was contamination in the magma evolution. Magmadifferentiation is demonstrated by variations of LREE and LILE from depletion to enrichment. Additionally, normalizedREE patterns and trace elements showed that lavas from the Bikou volcanic terrane have similar characteristics to those ofbasalts in arc settings caused by subduction and collision. Analyses showed that the Bikou volcanic terrane is a volcanicarc. New evidence proved that the Hengdan Group, north of the Bikou arc, is a turbidite terrane filling a forearc basin.Consequently, the Bikou volcanic terrane and the Hengdan turbidite terrane construct an arc-basin system. New SHRIMPages showed that this arc-basin system developed on the northern margin of the Yangtze craton in the Neoproterozoic(846-776 Ma), and this arc-basin system is in agreement with the tectonic processes of Rodinia in the Neoproterzoic. |
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| Keywords: | geochemistry Sr-Nd-Pb isotopes SHRIMP ages Bikou Volcanic Terrane southwestern Qinling Mts Yangtze Craton Rodinia |
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