Hotspot distribution, gravity, mantle tomography: evidence for plumes

Citation
E. Seidler et al., Hotspot distribution, gravity, mantle tomography: evidence for plumes, J GEODYN, 27(4-5), 1999, pp. 585-608
Citations number
74
Categorie Soggetti
Earth Sciences
Journal title
JOURNAL OF GEODYNAMICS
ISSN journal
02643707 → ACNP
Volume
27
Issue
4-5
Year of publication
1999
Pages
585 - 608
Database
ISI
SICI code
0264-3707(199905/07)27:4-5<585:HDGMTE>2.0.ZU;2-X
Abstract
Thermal convection is the motor of Earth dynamics and therefore is the link between plate motions, hotspots, seismic velocity variations in the mantle , and anomalies of the gravity field. Small scale mantle anomalies, such as plumes, do, however, generally escape detection by tomographic methods. It is attempted to approach the problem of detection in a somewhat statistica l manner. Correlations are sought between spherical harmonic expansions of the 'fields' under study: the hotspot distribution, mantle velocity variati ons, gravity, heat flow. Using spherical harmonic representations of global fields implies integration and averaging over the whole globe. Thus, altho ugh relationships may remain masked in the space domain by a multitude of e ffects, tendencies may become visible in the spectra or in appropriate aver ages. The main results are the following: There is a significant long wavelength (n=2,3) negative correlation between the hotspot density and the P-wave vel ocity variation in the lower mantle. Positive hotspot density of degree 2 t o 9 generally correlates with low seismic velocity in all depths of the upp er mantle and with positive gravity. This fits well with plume-type convect ion. These results are also confirmed regionally for a number of individual mid-ocean ridges and hotspots. The hotspot density and the free air anomal ies are distinctly positive above regions of low velocity extending to grea t depth. The effect is not distinct at ridges with shallow velocity anomali es. In a general way, we suggest that the antipodal upwellings (Pacific, Af rica) are divided by downwelling currents around the shrinking Pacific. Pla te boundaries can easily move away from their past connections with the dee per mantle. Small scale plume currents seem to be depicted in the hotspot e xpansion. (C) 1999 Elsevier Science Ltd. All rights reserved.