Page 3: Research news on mantle plume

A mantle plume is a buoyant, localized upwelling of anomalously hot, partially molten or near-solid-state mantle material that rises from depth toward the lithosphere, driven primarily by thermal and compositional density contrasts. In geodynamic models, mantle plumes are often represented as narrow, cylindrical conduits with bulbous heads, capable of producing large magma volumes upon decompression melting in the upper mantle. They are invoked to explain intraplate magmatism, flood basalt provinces, and hotspot volcanism, and are studied through seismic tomography, geochemical tracers (e.g., isotopic signatures), and numerical or analogue convection experiments that constrain their temperature excess, geometry, and temporal evolution.

Scientists detect deep Earth pulses beneath Africa

Research led by Earth scientists at the University of Southampton has uncovered evidence of rhythmic surges of molten mantle rock rising from deep within the Earth beneath Africa. These pulses are gradually tearing the continent ...

Evidence of a possible ghost plume beneath Oman

An international team of geoscientists, chemists and climate scientists, has found evidence of a possible ghost plume beneath the territory of Oman. In their paper published in the journal Earth and Planetary Science Letters, ...

page 3 from 3