Inhaltsbereich
Publications
(Co) Author: Smethurst, M. A.
(since 2006) [ All ]
-
(2008): Plume Generation Zones at the margins of Large Low Shear Velocity Provinces on the the Core-Mantle Boundary. Earth and Planetary Science Letters, 265, 1-2, 49-60.
-
(2008): Long term stability in deep mantle structure: Evidence from the ~ 300 Ma Skagerrak-Centered Large Igneous Province (the SCLIP). Earth and Planetary Science Letters, 267, 3-4, 444-452.
-
(2006): Large igneous provinces generated from the margins of the large low-velocity provinces in the deep mantle. Geophysical Journal International, 167, 3, 1447-1460.
TOP-
(2008): Implications for Long-Term Mantle History of the Restricted Distribution of Large Igneous Province (LIP) Plume Sources at the Core-Mantle Boundary (CMB). AGU 2008 Fall Meeting (San Francisco, USA 2008).| EDOC: 13583 |
-
(2008): Possible analogous long-term histories of the terrestrial geoid and the Martian aeroid. 39th Lunar and Planetary Science Conference (League City, TX, USA 2008).| EDOC: 13613 |
-
(2008): Supercontinents, Plate Tectonics, Large Igneous Provinces and Deep Mantle Heterogeneities. AGU 2008 Fall Meeting (San Francisco, USA 2008).| EDOC: 13587 |
-
(2007): Frequency distribution of seismic wavespeed as evidence for bodies of distinct material in the lowermost mantle, and analogies with the lithosphere. 24th IUGG 2007 (Perugia, Italy 2007).| EDOC: 13931 |
-
(2007): Long term stability in Deep Mantle structure: Evidence from the ~ 300 Ma Skagerrak-Centered Large Igneous Province (the SCLIP). General Assembly European Geosciences Union (EGU) (Vienna, Austria 2007).| EDOC: 13937 |
-
(2006): Plume Generation Zones (PGZs) at the Core-Mantle Boundary (CMB). AGU Fall Meeting (San Francisco, USA 2006).| EDOC: 13940 |
-
(2006): Structure within the D'' zone and the origin of LIPS. The 10th SEDI (Study of the Earth's Deep Interior) Symposium (Prague, Czech Republic 2006).| EDOC: 13956 |
-
(2006): SPlates: Palaeogeographic reconstruction software. NGU Report 2006.060, Statoil ASA.| EDOC: 14132 |