-
provinces (LLSVPs), also
called large low-velocity
provinces (LLVPs) or
superplumes, are
characteristic structures of
parts of the
lowermost mantle, the...
-
upwelling of
mantle material from the core–mantle boundary,
referred to as
superplumes. Two
present day
superswells have been identified: the
African superswell...
- in
favor of
mantle plumes beneath the EAR.
Others proposed an
African superplume causing mantle deformation.
Although the
effects of deep-rooted mantle...
- America: a
first order continental structure generated by the
Cretaceous superplume mantle event".
Journal of Geodynamics. 34 (2): 163–176. Bibcode:2002JGeo...
- due to the
large feature size they image, such as
subducted slabs and
superplumes. The
trade off from
whole mantle to
whole Earth coverage is the co****...
- Maruyama, Shigenori; Karato, Shun-Ichiro; Windley,
Brian F., eds. (2007).
Superplumes:
Beyond Plate Tectonics. Dordrecht,
South Holland: Springer. ISBN 978-1-4020-5749-6...
- A
superplume generated by
cooling processes in the mantle....
-
supercontinent Rodinia began to
break up 870–845 Ma
probably as a
consequence of a
superplume caused by
mantle slab
avalanches along the
margins of the supercontinent...
- centre.
Plumes derived from a
superplume (or
Large Low
Shear Velocity Province (LLSVP))
overlay the
boundary of the
superplume at the core-mantle boundary...
-
subduction of the Kula and
Pacific plates,
which was
probably caused by a
superplume.
During the
opening of the
South Atlantic the Paraná–Etendeka LIP produced...
