Garnet-controlled very low velocities in the lower mantle transition zone at sites of mantle upwelling
Author:
Affiliation:
1. Department of Geoscience; Aarhus University; Aarhus Denmark
2. Department of Geoscience; Christian-Albrechts University; Kiel Germany
3. Department of Earth Sciences; Durham University; Durham UK
Funder
Aarhus Universitets Forskningsfond
Carlsbergfondet
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/ter.12348/fullpdf
Reference53 articles.
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3. The isolation of receiver effects from teleseismic P waveforms;Ammon;Bulletin of the Seismological Society of America,1991
4. Detailed nature of the 660 km region of the mantle from global receiver function data;Andrews;Journal of Geophysical Research: Solid Earth,2008
5. Phase transition Clapeyron slopes and transition zone seismic discontinuity topography;Bina;Journal of Geophysical Research,1994
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