LINKS BETWEEN LONG‐LIVED HOT SPOTS, MANTLE PLUMES, D″, AND PLATE TECTONICS

196 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

Convective patterns under the Indo-Atlantic « box » (2005, methodology): “Laboratory experiments are shown in red [85], dark blue [86], yellow [ 69 ] and black [57,59,61,62,67].”
Conditions for the onset of plate tectonics on terrestrial planets and moons (2007, background): “The elastic lithosphere for old oceanic lithosphere on Earth is ∼40 km (Calmant et al., 1990; Watts and Burov, 2003; Jellinek and Manga, 2004; McNutt, 2004).”
Postperovskite phase transition and its geophysical implications (2006, background): “Part of the geochemical variations found in plume-related magmas could be formed by melting at the CMB [e.g., Jellinek and Manga, 2004; Hirose et al., 2004].”
Thermal versus elastic heterogeneity in high‐resolution mantle circulation models with pyrolite composition: High plume excess temperatures in the lowermost mantle (2009, background): “[49] An important argument in support of chemical heterogeneity is the morphology, or shape, of deep mantle upwellings, taken either from direct observations of seismic data [Ni et al., 2002], or from laboratory [Jellinek and Manga, 2004] and numerical studies [McNamara and Zhong, 2004].”