Mathematics – Logic
Scientific paper
Aug 1992
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992e%26psl.112..179v&link_type=abstract
Earth and Planetary Science Letters, Volume 112, Issue 1, p. 179-194.
Mathematics
Logic
25
Scientific paper
Recent laboratory work has suggested that the rheology of the lower mantle may be Newtonian. We have studied the time-dependent dynamics of plumes interacting with a rheological interface separating an upper non-Newtonian mantle and a Newtonian lower mantle. Pulsating diapiric structures with fast time scales are promoted by the interaction of the rising plumes with this rheological boundary. Surface heat flow signals are discernible as pulses, which remain relatively stationary. They correlate well with the localized upwellings just below the surface. The presence of a mobile lithosphere from increasing the non-Newtonian power-law index helps to produce a large-scale circulation in the upper mantle which draws large hot patches away from nearby upwellings. In our calculations the resultant averaged effective viscosity of the non-Newtonian upper mantle is about two orders of magnitude lower than that of the Newtonian lower mantle. A viscously stratified Newtonian model produces more incoherent and broad-scale diapiric structures and is less efficient for generating sharply varying time-dependent thermal signatures.
van den Berg Arie
van Keken Peter
Yuen David A.
No associations
LandOfFree
Pulsating diapiric flows: Consequences of vertical variations in mantle creep laws does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Pulsating diapiric flows: Consequences of vertical variations in mantle creep laws, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Pulsating diapiric flows: Consequences of vertical variations in mantle creep laws will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-1166625