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What is Hardmanetal 2018JGSLProlongeddynamicsupport about?
The article discusses the prolonged dynamic support from the Iceland mantle plume affecting the NE Atlantic margin, particularly focusing on the Faroe-Shetland Basin. It documents the stratigraphic record of subsidence following uplift around 56 Ma, revealing a complex history of uplift and subsequent subsidence, with significant implications for understanding the duration of dynamic support. The findings suggest that palaeogeographical analysis can effectively constrain the timing and mechanisms of dynamic
- Author
- Som Dev
- Language
- EN