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Tristan hotspot
Three Hotspot Reference Frames – Shallow and Lithospherically Controlled – Reflect “Mesoplates”, a Plate Tectonics Heuristic
Aula 4 – Tipos Crustais Tipos Crustais Continentais E Oceânicos
An Interdisciplinary Approach to Volcanic Risk Reduction on Tristan Da Cunha
Insights Into the Origin and Evolution of Intraplate Magmatism in the Caribbean
Sleep, N.H., Hotspots and Mantle Plumes: Some Phenomenology, J
Cretaceous Paleomagnetic Field in North America: True
Back Matter (PDF)
Primitive Helium Is Sourced from Seismically Slow Regions in The
Hot Upper Mantle Beneath the Tristan Da Cunha Hotspot from 10.1002/2017GC007347 Probabilistic Rayleigh-Wave Inversion and Petrological
A Biophysical Profile of the Tristan Da Cunha Archipelago (PDF)
Report from the Hotspot Geodynamics Detailed Planning Group
The Magmatic System Beneath the Tristan Da Cunha Island: Insights from Thermobarometry, Melting Models and Geophysics
Primordial Helium Entrained by the Hottest Mantle Plumes M
Hotspots, Mantle Plumes, Flood Basalts, and True Polar Wander
Spatial Characteristics of Recycled and Primordial Reservoirs in the Deep Mantle
Hot Upper Mantle Beneath the Tristan Da Cunha Hotspot from Probabilistic Rayleigh-Wave Inversion and Petrological Modeling
Becker, T. W., & Advance Our Understanding of Deep Mantle Reservoir Distributions, and We Discuss How Continental and Steinberger, B
How and When Plume Zonation Appeared During the 132&Thinsp
Top View
The Onset of Walvis Ridge: Plume Influence at the Continental Margin
Ocean Drilling Program Scientific Results Volume
Fromm, T., L. Planert, W. Jokat, T. Ryberg, J. H. Behrmann, M.H. Weber, and Christian Haberland, South
Earth and Planetary Science Letters 414 (2015) 156–163
Downloaded from of the LLSVP by Primary Plume Heads Triggered Upwelling of HIMU Material from a More Internal Domain of the LLSVP, Forming Secondary Plumes
Absolute Plate Motions in a Reference Frame Defined by Moving Hotspots
Hafnium Isotope Ratio in Mid-Ocean Ridge Basalts: a Global Survey and a Focus on the Southern Mid-Atlantic Ridge (40°S - 55°S)
Tectonically Restricted Deep-Ocean Circulation at the End of the Cretaceous Greenhouse
A Compositional Anomaly at the Earth's Core–Mantle Boundary As