The Lower Cretaceous Giant Dyke Swarms in the Arctic and Its Significance for linking of Siberia-Iceland Hot-Spot Track

Siberia-Iceland hot-spot track is the one of hot-spot track preserved on continent.Although this hot-spot track has clear plume"heads"-Siberia large igneous province,owing to thick continental lithosphere,its continuing magmatism associated with remaining plume"tail"is unclear co...

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Bibliographic Details
Main Authors: LIU Zhonglan, LI Jianghai, ZHANG Huatian
Other Authors: The Key Laboratory of Orogenic Belts and Crustal Evolution,School of Earth and Space Sciences,Peking University
Format: Conference Object
Language:English
Published: 第七届国际岩墙会议——“岩墙群:超大陆重建的钥匙” 2016
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Online Access:https://hdl.handle.net/20.500.11897/479892
Description
Summary:Siberia-Iceland hot-spot track is the one of hot-spot track preserved on continent.Although this hot-spot track has clear plume"heads"-Siberia large igneous province,owing to thick continental lithosphere,its continuing magmatism associated with remaining plume"tail"is unclear compare to other typical hot-spot track occurs in Siberia-Iceland hot-spot track is the one of hot-spot track preserved on continent.Although this hot-spot track has clear plume"heads"-Siberia large igneous province,owing to thick continental lithosphere,its continuing magmatism associated with remaining plume"tail"is unclear compare to other typical hot-spot track occurs in 中国科学院地质与地球物理研究所 1 Vol.90