Plumes, hotspots and the CMB - PowerPoint PPT Presentation

1 / 27
About This Presentation
Title:

Plumes, hotspots and the CMB

Description:

B = -4 r3g /3 =c v/r; R= r c. v Forces on the sphere balanced velocity constant. B R=0 V= -g r2/3c. If viscosity of sphere and surrounding different. c ... – PowerPoint PPT presentation

Number of Views:46
Avg rating:3.0/5.0
Slides: 28
Provided by: carolinali
Category:
Tags: cmb | hotspots | plumes

less

Transcript and Presenter's Notes

Title: Plumes, hotspots and the CMB


1
Plumes, hotspots and the CMB
  • Lecture 6 Geodynamics
  • Carolina Lithgow-Bertelloni

2
Earths temperature profile
3
Scales of Convection
from Geoff Davies
4
Plumes and Hotspots
  • Hotspots
  • Island chains and age progression
  • Importance for plate motions, TPW
  • Fixity
  • Chemistry
  • Origin
  • Plumes
  • Difference with large-scale upwellings
  • Heads and tails
  • Effects of viscosity on morphology
  • Plume initiation and flood basalts
  • How much entrainment
  • Comparison to geochemistry
  • Effects of composition
  • Shape, heterogeneity, hotspot fixity
  • Relationship between large-scale upwellings and
    plumes?
  • Capture by plate-scale flow
  • Consequences for heat flow
  • Where do they come from?

5
Hotspots
  • Concentrated volcanic activity.
  • Linear volcanic chains in the interiors of the
    plates.
  • Age progression along chain
  • Chemistry of erupted lavas is significantly
    different than MOR or IA
  • Some hotspots have broad topographic swell 1000
    m

Steinberger et al., 2004
6
Hotspots and Plates
25-43 Ma
43-48 Ma
7
Hotspots, fixity and plate motions
8
Hotspot fixity and mantle wind
Steinberger et al., 2004
9
Chemistry
Barfod et al., 1999
10
Plumes and hotspots
  • Rayleigh-Taylor instability
  • Large head, thin tail
  • Rheology
  • Vigor of convection
  • Compositional vs thermal buoyancy
  • Ascent times
  • Rheology
  • Deflection, capture by mantle wind
  • Compositional vs thermal buoyancy

Griffiths and Campbell, 1990
11
Rise time estimate
r 500 km ???????????? ????????? ? V 80 km/My
r
v
??
Ratio of buoyancy force to viscous forces B
-4?r3g??/3 ??c?v/r R???r c?v Forces on the
sphere balanced velocity constant BR0 V
-g??r2/3c? If viscosity of sphere and
surrounding different c ?????????/ ?????? c
1-1.5
12
Generating a mantle plume
from Geoff Davies
13
Large-scale upwellings and plumes
Boschi and Dziewonski,1999
Ni et al.,2002
14
Plume morphology effects of viscosity
Whitehead and Luther, 1975
15
Plumes heads and tails
Lithgow-Bertelloni et al., 2001
16
Head Tail Radii
Lithgow-Bertelloni et al., 2001
17
Thermochemical Plumes
Farnetani, 2004
18
Entrainment and mixing
19
Plumes and geochemical heterogeneity
Samuel and Farnetani, 2003
20
Evolution of heterogeneity
LeBars and Davaille, 2004
21
Plumes and large-scale upwellings
Davaille, 2000
22
Thermochemical plumes and fixity
Jellinek and Manga, 2002
23
Plume capture by large-scale flow
Jellinek et al., 2002
?? and Pe control BLT and Q ?????????
(Pe?)1/3 ???????? Q (Pe)1/2
V and ???hot/?int No effect Vltlt 1 ?
1 Suppression Vgt 10 ? gt 100 Sweeping V
intermediate f(??
24
Where do plumes originate?
Davaille, 2000
25
The plume source region CMB
Sidorin et al., 1999
26
Plume Frequency 3 Different Experiments
27
Episodic Crustal Production?
Condie, 1998
Write a Comment
User Comments (0)
About PowerShow.com