Roadmap | The website review process | Home
:: MECHANISMS ::  Ridge-transform intersections Impacts Plate tectonic processes Reheated slabs Gravitational instability EDGE
  Earth tessellation Rifting decompression meltingSlab breakoff PLATEHydration weakening Plumes Small-scale convection Shear-driven upwelling
:: LOCALITIES ::
Mantle heterogeneity
Zombie science
Olivine control temperatures
Recycling
Titanium
Tomography problems
Hell
Transition zone
Mantle warming
Plumes
Plume coffin
Self-organization
LIP classification
Osmium & tungsten
Lithospheric uplift
Lower crust recycling
Origin of OIB
Eclogite reservoirs
Norwegian volcanic margin
Volcanic margins
Silicic LIPs
Metasomatic OIB
What is a plume?
Komatiites
Neon & Argon
Thermal
Mantle temperature under LIPs
Ar-Ar dating
Pacific seamount ages
Hotspot table
Radiating volcanic migrations
Giant dikes
Cracks & stress
Plumes exist because...
Convection
Hotspot reference frame
Seismology
Noble gases
Pt-Os
Mantle reservoirs
General theory of plate tectonics


Localities : Africa | Antarctica | Atlantic | Central America | Eurasia | Iceland & Greenland | India | North America | Pacific | Planetary | South America

:: A glance at today's paper ::  

Obrebski, M.; Allen, R.M.; Xue, Mei; Hung, Shu-Huei, Slab-plume interaction beneath the Pacific Northwest, Geophys. Res. Lett., 37, No. 14, L14305, 2010.



Recent scholarly articles


Popular magazine articles


Foundations


Volcanic margins


Related links



The P^3 Book



Bibliographies & papers

:: Notice Board:

AGU Sessions

V37: Are Hotspots Hot?
T11: The Global Low Velocity Zone
V25: Generation and Evolution of Alkaline to Sub-alkaline Magmas


Can tomography detect plumes? Discussion


Implications for melt in the upper mantle from the electrical conductivity of melt-bearing peridotites at high pressures

T. Yoshino, M.l Laumonier, E. McIsaac & T. Katsura


The pulsing Iceland plume: A personal evolution from believer to agnostic

R. Hey


Plates vs Plumes:
A Geological Controversy

Gillian R. Foulger

ISBN: 978-1-4051-6148-0
Paperback, 352 pages
September 2010
Wiley-Blackwell

£32.50 / €37.40 / $65.00


Southern African topography and erosion history:
plumes or plate tectonics?

A. Moore, T. Blenkinsop & F. Cotterill


Updated webpage:

Shallow magma sources during continental rifting and breakup of the South Atlantic

D. Franke, K. Hinz, S. Ladage, S. Neben, M. Schnabel, B. Schreckenberger


V-shaped ridges on the Reykjanes Ridge:
Plume pulses not required:

Hey et al., Propagating rift model for the V-shaped ridges south of Iceland, G3, 11, 2010.



Total number of visitors to date:

(Click me)
 


P^4 Book


Slide shows


Conferences

Cruises


LIPs


Planetary


Talk about plumes


Plume coffin

Any questions? Any Comments? Want to contribute? | About this site


:: Comments::

:: Comments? Questions?::
email the website manager


MantlePlumes.org mugs. To order, click here

 

23rd April, 2010
Dear WM, There have been numerous ad hoc attempts to explain why bathymetry violates the square-root-age relation after 70 Ma but none of them are consistent with the continued growth of the seismic lid across the whole Pacific. The latest attempt to unflatten the seafloor is in the issue of Science that hit the stands on April Fools Day 2010 but has a publication date one day later. I discuss the flattening problem in the attached document.–Don Anderson


22nd April, 2010
The process by which science advances is a conservative one. That is, each step of the way involves documentation that the new information is reproducible and consistent with the existing body of knowledge. For most day-to-day operations of science, this approach is reasonable and successful; inaccurate observations and incorrect deductions are weeded out, and accurate observations and deductions are added to the fabric of knowledge. However, when new observations or arguments do not fit into the existing paradigm, there is a strong tendency for them to be rejected by the scientific community. The larger the shift of paradigm required to accommodate the new information, the more harsh and emotional is likely to be the rejection.–Harry W. Green, from "Psychology of a Changing Paradigm"


::more::

 

:: HOME :: MECHANISMS :: LOCALITIES :: GENERIC ::
© MantlePlumes.org