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Titlebook: Oceanic Hotspots; Intraplate Submarine Roger Hekinian,Jean-Louis Cheminée,Peter Stoffers Book 2004 Springer-Verlag Berlin Heidelberg 2004 I

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A Global Isostatic Load Model and its Application to Determine the Lithospheric Density Structure o motion of about 100 km thick lithospheric plates that were gliding on their substratum, the asthenosphere. The dynamics of the plates, thought to be driven by convection currents in the asthenosphere, determines the relief of the Earth’s crust.
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The Foundation Chain: Inferring Hotspot-Plate Interaction from a Weak Seamount Trail,/Del Cano and Chile FZs Fig. 11.2. A segment of the Nazca plate was transferred to the Pacific Plate during this period of reorganization to form the short-lived Selkirk Microplate Fig. 11.2 (.; .; .) via a spreading-ridge propagation event between chron 6C (23.4–24 Ma) and Chron 6(0) (20.2 Ma) (.).
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The Sources for Hotspot Volcanism in the South Pacific Ocean,1). During the last fifteen years, the German-French initiative to study these hotspots has resulted in a vast amount of petrological and geochemical data being collected on fresh, mainly submarine volcanics.
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