Iceland Plume and its Magmatic Manifestations:LIP-Dornr?schen in the North Atlantic  

作　　者：Sierd CLOETINGH Alexander KOPTEV 

机构地区：[1]Department of Earth Sciences,Utrecht University,Netherlands [2]GFZ German Research Centre for Geosciences,Potsdam,Germany

出　　处：《Acta Geologica Sinica(English Edition)》2024年第S01期10-10,共1页地质学报（英文版）

摘　　要：Plume-lithosphere interactions are key in the coupling of deep Earth and surface processes,impacting deformation and evolution of sedimentary basins and continental topography at different spatial scales(Cloetingh et al.,2022,2023).The North Atlantic region is a prime example of the interaction between plate tectonic movements and thermal instabilities in the Earth's mantle.The opening of the Labrador Sea/Baffin Bay and the North Atlantic,the widespread volcanism and the localized uplift of the topography in Greenland and the North Atlantic are traditionally attributed to the thermal effect of the Iceland mantle plume.

关 键 词：plume-lithosphere interaction large igneous provinces Iceland Plume 

分 类 号：P542[天文地球—构造地质学] P736[天文地球—地质学]