Inhaltsbereich
Publications
(Co) Author: Priestley, K.
(since 2005) [ All ]
| Paper (ISI journals) [7] |
Conference Paper [6] |
All [13] |
-
(2012): Crustal structure of the British Isles and its epeirogenic consequences. Geophysical Journal International, 190, 2, 705-725.
-
(2010): Rayleigh wave phase velocity maps of Tibet and the surrounding regions from ambient seismic noise tomography. Geochemistry Geophysics Geosystems (G3), 11, Q08010.
-
(2009): Relationship between the upper mantle high velocity seismic lid and the continental lithosphere. Lithos, 109, 1-2, 112-124.
-
(2008): Variations of shear-wave splitting in Greenland: Mantle anisotropy and possible impact of the Iceland plume. Tectonophysics, 462, 1-4, 137-148.
-
(2007): Crustal structure of Iceland and Greenland from receiver function studies. Journal of Geophysical Research, 112, B03301.
-
(2006): Lithospheric structure of the Aegean obtained from P and S receiver functions. Journal of Geophysical Research, 111, B12307, 1-23.
-
(2005): The lithosphere-asthenosphere boundary in the North-West Atlantic region. Earth and Planetary Science Letters, 236, 1-2, 249-257.
TOP-
(2012): Velocity structure of the NE Tibetan Plateau: P and S body wave tomographic model of the northeastern Tibetan Plateau and its margins with additional constraints from surface wave tomography. AGU 2012 Fall Meeting (San Francisco, USA 2012).| EDOC: 20096 |
-
(2011): P- and S-wave tomographic structure of NE Tibet. AGU 2011 Fall Meeting (San Francisco 2011).| EDOC: 18077 | Abstract |
-
(2011): P-wave tomographic structure of NE Tibet. General Assembly European Geosciences Union (Vienna, Austria 2011).| EDOC: 20563 | Abstract |
-
(2011): High resolution 3D Sv wave velocity model of China and surrounding area. AGU 2011 Fall Meeting (San Francisco 2011).| EDOC: 18067 | Abstract |
-
(2006): Shear wave splitting varations in Greenland. 3rd General Assembly European Geosciences Union (Vienna, Austria 2006).| EDOC: 11267 |
-
(2005): Lithospheric structure in the Aegean area and Greece obtainded from P and S receiver function methods. 2nd General Assembly European Geosciences Union (Vienna, Austria 2005).| EDOC: 7290 | Abstract |